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U.S. GEOLOGICAL SURVEY
SAUDI ARABIAN MISSION
TECHNICAL RECORD 17
(INTERAGENCY REPORT 372)
IRON SULFIDE DEPOSITS AT WADI WASSAT,
KINGDOM OF SAUDI ARABIA
by
Ralph J. Roberts, Darwin L. Rossman,
Abdulaziz Y. Bagdady, Clay M. Conway, and Abdul Malik Helaby
U.S. Geological Survey Open-File Report §£ /%
This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards.
U.S. Geological Survey Jiddah, Saudi Arabia
1981
The work on which this report was based was performed in accordance with a cooperative agreement between the U.S. Geological Survey and the Ministry of Petroleum and Mineral Resources.
The report has not been edited or reviewed for conformity with U.S. Geological Survey standards and nomenclature. Product names used in this report are for descriptive purposes and in no way imply endorsement by the U.S. Geological Survey.
The quadrangle identification method used in U.S. Geological Survey Saudi Arabian Mission reports is shown below.
41°23°
41°
23/41
1 -degree quadrangle
23/41 B
30-minute quadrangle
CONTENTS
Page
ABSTRACT............................................... 1INTRODUCTION........................................... 2
Location........................................... 2Previous work...................................... 2Present investigation .............................. 4
GEOLOGY OF THE WADI WASSAT AREA........................ 4Introduction....................................... 4Sedimentary, pyroclastic, and volcanic rocks....... 5
Mahal formation ............................... 7Wassat formation .............................. 7Duwayr formation .............................. 8
Intrusive rocks.................................... 8Dike rocks .................................... 9
Alluvium........................................... 9STRUCTURE.............................................. 9IRON SULFIDE DEPOSITS.................................. 12
Introduction....................................... 12Origin of the deposits at Wadi Wassat.............. 15Sampling program................................... 19Description of the deposits........................ 21
Area A gossan ................................. 21Drill hole WS-1.......................... 21Drill hole WS-5.......................... 25
Area B gossan ................................. 25Drill hole WS-3.......................... 25Drill hole WS-4. ......................... 32
Area C........................................ 32Area D........................................ 32Area E........................................ 32
Drill hole WS-7.......................... 36Area F........................................ 36
Drill hole WS-6.......................... 36Area G gossan ................................. 36Area H gossan ................................. 36
Drill hole WS-8. ......................... 41Area I gossan ................................. 41
Drill hole WS-9.......................... 41Area J gossan ................................. 48Area K gossan ................................. 48Area L........................................ 48
Geochemistry....................................... 48Results of analytical work.................... 49
Resources.......................................... 49REFERENCES CITED....................................... 52
ill
APPENDIX 1.
2.
Gossan sample areas, sample numbers,and assays.............................
Diamond drill hole data, list of samples, and assays of core samples.............
Page
55
90
Plate
ILLUSTRATIONS [Plate is in pocket]
Geologic map of Wadi Wassat iron sulfide deposits
Figure 1. Index map showing location of iron sulfidedeposits at Wadi Wassat................... 3
2. Generalized geologic map showing trace ofthe mineralized zone ...................... 6
3. Detailed map showing structure in the vicinityof drill holes WS-6, -7, and -8........... 11
4. Geologic map of thrust fault zone neardrill hole WS-9........................... 13
5. Photographs and photomicrographs ofsulfide ore ............................... 16
6. Cross sections along drill holes WS-1, -5,-3, -4, -6, -7, -8, and -9................ 22
TABLES
Table 1. Summary of analytical results from 272gossan samples............................ 20
2. Depth of oxidation in the area.............. 213. Summary log of drill hole WS-1.............. 244. Analyses of core from drill hole WS-1....... 265. Summary log of drill hole WS-5.............. 276. Analyses of core from drill
hole WS-5................................. 287. Major element chemical analyses of core
from drill hole WS-5...................... 298. Summary log of drill hole WS-3.............. 309. Analyses of core from drill hole WS-3....... 3110. Summary log of drill hole WS-4.............. 3311. Analyses of core from drill hole WS-4....... 3412. Major element chemical analyses of core
from drill hole WS-4...................... 3513. Summary log of drill hole WS-7.............. 3714. Analyses of core from drill hole WS-7....... 3815. Summary log of drill hole WS-6.............. 39
IV
Page
1G. Analyses of core from drill hole WS-6....... 4017. Summary log of drill hole WS-8. ............. 4218. Analyses of core from drill hole WS-8....... 4319. Major element chemical analyses from
drill hole WS-8........................... 4420. Summary log of drill hole WS-9.............. 4521. Analyses of core from drill hole WS-9....... 4622. Major element chemical analyses of core
from drill hole WS-9....................... 4723. Distribution of pyrite and pyrrhotite in
drill holes WS-1 through WS-9............. 50
IRON SULFIDE DEPOSITS AT WADI WASSAT,
KINGDOM OF SAUDI ARABIA
by
Ralph J. RobertsjL/ , Darwin L. Rossman^/, Abdulaziz Y. Bagdady, Clay M. Conwayl/, and
Abdul Malik Helaby
ABSTRACT
Massive and disseminated iron sulfide deposits in Wadi Wassat form lenticular, stratabound deposits in cherty Precambrian sedimentary rocks interlayered with Precambrian calcareous sedimentary rocks, pyroclastic rocks, and an- desitic flow rocks. These rocks have been cut by a wide variety of plutonic and dike rocks including gabbro, diorite, granodiorite, diabase, rhyolite, and granite.
The zone containing the sulfide lenses is nearly 16 km long and is cut off by granitic rocks at both the northern and southern ends. The lenses are as much as 200 m thick; one can be traced along strike for more than 4 km. The lenses consist mostly of iron sulfides. Pyrite is the principal sulfide mineral; near intrusive bodiesj the pyrite has been partially converted to pyrrhotite and locally mobilized into fractures. The sulfides have been oxidized to a depth of about 25 m.
Preliminary calculations indicate that about 107,500,000 tons of sulfides, averaging 40 percent iron and 35 percent sulfur, are available to a depth of 100 m. Small amounts of nickel, cobalt, zinc, and copper are also present, but at metal prices prevailing in early 1981, these do not con stitute significant resources.
I./ U.S. Geological Survey, Menlo Park, California, U.S.A 2/ U.S. Geological Survey, Reston, Virginia, U.S.A.
INTRODUCTION
Location
The Wadi Wassat iron sulfide deposits are located in the southwestern part of the Kingdom of Saudi Arabia, in the Wadi Wassat quadrangle (sheet 18/44 C) , which is between lat 18°00' and 18°30'N., long 44°00' and 44°30'E., (fig. 1). The deposits crop out in Wadi Wassat, which drains northeast into the Rub al Khali; ridge-top altitudes are about 1,400 m above sea level .
The area can be reached by an unimproved road that ex tends from Bishah via Tathlith about 460 km southwestward to Najran. The area is 330 km southeast of Bishah and 130 km north of Najran; B'ir Idimah, the only permanent settlement in the area, is located about 30 km north of the deposit.
Previous work
The Wadi Wassat quadrangle was first mapped as part of the 1:500,000-scale Asir quadrangle by Brown and Jackson (1959). The first mineral exploration in the Wadi Wassat area was carried out by Hatem El-Khalidi of the Arabian Shield Development Company, a division of Dallas Resources Incorporated, who discovered the gossan at Wadi Wassat in October 1964. In the subsequent 3 years, W.C. Overstreet and others conducted studies of the economic geology along a series of traverses through the region (Overstreet 1968v 196#fei, &, i; Overstreet and others, 196?a, Overstreet and others, 196ty>; Overstreet and others, 1967b; and Overstreet and others, 1967£) .
Overstreet and Rossman (1970) carried on reconnaissance geologic mapping (scale 1:100,000) in the greater Wadi Wassat region, and Rossman mapped the gossan area in Wadi Wassat at a scale of 1:10,000 (written commun., 1967) This work was followed by electromagnetic ground geophysical studies (Alien and Davis, 196^a, b; Akhrass, 1966). In 1967-1969 a diamond drilling program was carried out under the supervision of Overstreet, Rossman, and Martin; nine holes totaling 1,100 m in length were completed. Martin (1973) also continued de tailed mapping in the area during 1968-1969.
During the late stages of the exploratory work, A.E. Weissenborn and R.L. Earhart visited the Wadi Wassat area and prepared a summary appraisal and an estimate of the resources in the deposits (Weissenborn and Earhart, 196^).
In 1968-1969 Barry Jackaman carried on detailed geologic studies in Wadi Wassat (1972). Greenwood (1980) mapped the Wadi Wassat quadrangle at a scale of 1:100,000.
36
16
36'
Figure 1.- Index map showing location ofWassat quadrangle, Kingdom of Saudi Arabia.
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Wadi Wassat, Wadi
Present investigation
This study is part of a broad program of mineral ex ploration conducted by the U.S. Geological Survey (USGS) in accordance with a work agreement with the Ministry of Petroleum and Mineral Resources, Kingdom of Saudi Arabia.
The objectives of the present study were to remap the gossans and adjacent host rocks in Wadi Wassat, resample mineralized zones, and evaluate the potential of the area for base metal and nickel deposits. Roberts and Bagdady were in the field from 13 March to 9 April 1975, revising the geologic map near the gossans and resampling some gossans. Helaby relogged the drill cores and supervised resampling of the cores. Conway spent a week with Roberts in 1977 assisting in evaluation of stratigraphic and structural features.
This report incorporates material from a draft initially prepared by Rossman that was revised and modified by W.C. Overstreet in 1972. Summary logs of drill holes and analy tical data initially compiled by Rossman are included in this report.
The writers gratefully acknowledge support and helpful cooperation received from H.E. Ghazi H. Sultan, Deputy Minister for Mineral Resources, and other officials of the Directorate General of Mineral Resources (DGMR). Appreci ation is also extended to K.J. Curry and chemists of the USGS-DGMR Chemical Laboratory for detailed analyses of samples and to Mohammed Naqvi for spectrographic studies of mineralized rock. Ghanim Jeri al Harbi, Merdhi al Mutairi Almotteir, Saud Mulish Alshabani, and Mugeeth Abdullah Algahtani assisted in the field studies. J. Matzko and M. Ma wad supervised preparation of polished specimens and photo graphed the sulfides and rocks. T. Hopwood, consultant for Riofinex Limited, contributed useful structural and strati- graphic information .D.LSchmidt assisted Roberts and Conway in evaluating stratigraphic and structural features.
R.M. Nixon conducted surveys that tied the area into the Saudi Arabian national geodetic net; F.J. Fuller and D.J. Faulkender calculated the latitude and longitude of a station within the mapped area; Faulkender also calculated the area of the gossan for resource computations.
GEOLOGY OF THE WADI WASSAT AREA
Introduction
The geology of the Wadi Wassat quadrangle was first de scribed by Overstreet and Rossman (1970); they assigned the
rocks in the area to an unnamed Precambrian sequence of un met amorphosed to metamorphosed interlayered volcanic and sedimentary rocks. Jackaman (1972) later divided these rocks into three units, the Duwayr group, the Wassat group, and the Mahal group. He placed the contact between the Duwayr and Wassat groups 50-200 m east of the principal iron sulfide- bearing unit. This contact is a distinctive lithologic break, and we have followed Jackaman's usage.
Greenwood (1980) combined Jackaman's (1972) Duwayr group, Wassat group, and the eastern part of the Mahal group into a redefined Wassat formation and renamed the western part of Jackaman's Mahal group as the Qatan formation. He placed these two formations in the Jiddah group. We prefer to fol low the nomenclature of Jackaman, which is based on detailed studies and has priority. However, in keeping with Article 9 of the Code of Stratigraphic Nomenclature (Cohee, 1974), which requires that a group contain two or more formations, we recommend that Jackaman's units be reduced to formational status: that is, Wassat, Duwayr, and Mahal formations.
While resampling was being done in the Wadi Wassat dis trict during early 1975, the gossans and immediately adjacent wall rocks were remapped in places. During the course of this work, several observations of graded bedding and truncated beds in the upper part of the Wassat formation (near point a on fig. 2, approximate lat 18°22'N., long 44°13'E.) indicated that the Stratigraphic tops of beds are to the east. These observations were confirmed by T. Hopwood (oral commun., 1978), who measured cleavage intersections with bedding in the Wassat and adjacent Duwayr formations in the same area. Therefore, the Duwayr formation is apparently the youngest rather than the oldest of the three formations in the area. In addition, bedding and foliation attitudes and truncated beds near point b on figure 2 suggest that the iron sulfide unit is folded into an anticline-syncline pair that plunges steeply south. The positions of the syncline on the west and the anticline on the east also indicate that the Stratigraphic tops are to the east. So, although we accept Jackaman's (1972) formations, their order in the following account will be reversed to reflect our understanding of their relative ages.
Sedimentary, pyroclastic, and volcanic rocks
The sedimentary, pyroclastic, and volcanic rocks that contain the iron sulfide-bearing beds in the Wadi Wassat area were divided by Jackaman (1972) into three units: a unit of sedimentary and pyroclastic rocks (Mahal formation); a unit of sedimentary, pyroclastic, and volcanic rocks containing iron sulfide-bearing layers (Wassat formation); and a unit of pyroclastic and volcanic rocks (Duwayr formation) .
SA(IR)-372
EXPLANATION
Alluvium
Granitic rocks
Diorite
Duwayr Formation
' Wassat Formation (gossan zone (g) near top of unit)
Mahal Formation
Contact _ dashed where approximately located; dotted where concealed
Fault _ dashed where approximately located; dotted where concealed; arrows show relative displacement
Thrust fault _ dashed where approximately located; dotted where concealed
18 22'
Figure 2.- Generalized geologic map showing trace of the mineralized zone. Capital letters refer to gossan areas as described in text; roman numerals indicate ore zone segments, a. Area of east-facing beds in upper part of Wassat formation and lower part of Duwayr formation, b. Syncline in Wassat formation.
The sedimentary and volcanic rocks in Wadi Wassat were regionally metamorphosed to greenschist facies and are now characterized by sericite, chlorite, epidote, and locally graphite. In places, biotite schist and hornblende schist have formed in areas adjacent to or near plutonic rocks.
Mahal formation
The Mahal formation consists of andesitic pyroclastic rocks, rhyodacitic tuff, wacke, and minor amounts of marble (Jackaman, 1972). This unit ranges from 500 to 2,000 m thick and underlies the western part of the area 2>h?£.<j*^ on the plate. It is well exposed on the margins of Wadi Mahal, where it crops out in subparallel north-trending strike ridges. The upper beds of the Mahal formation grade into the overlying Wassat formation.
Locally, the Mahal formation contains lenses of iron sul- fide minerals that are now oxidized to gossans at the sur face. These lenses are thin, ranging from less than a meter to as much as 5 m^/cA<)verstreet and Rossman (1970, pi. 1) noted the presence of similar sulfide-bearing beds west of the mapped area and in other parts of the Wadi Wassat quadrangle .
Wassat formation
The Wassat formation comprises interlayered sedimentary, pyroclastic, and volcanic rocks, and iron sulfide-bearing units, which were estimated by Jackaman (1972) to aggregate as much as 5,000 m in thickness in the mapped area (plate). The thick volcanic and pyroclastic units of the lower and middle parts of the formation form bold outcrops in the rug ged upland between Wadi Mahal and Wadi Wassat. The iron sulfide-bearing units in the upper part generally weather readily to iron oxide gossans, forming valleys in most places; some siliceous gossans crop out as prominent ridges.
The lower beds of the Wassat formation include interbed- ded wacke, sandstone, siltstone, impure limestone, and tuff- aceous rocks. The middle part includes pyroclastic rocks, volcanic flows, and some coarse clastic units; the pyro clastic rocks include interlayered tuff, breccia, and locally thick agglomerate. The upper part contains some thin andesitic flows, pyroclastic rocks, and calcareous tuff, which are capped by laminated pyritic chert and tuff and intercalated iron sulfide lenses, now altered to gossan. The gossans crop out in a zone that is as much as 560 m wide. The gossans consist of iron oxides and secondary silica interlayered with laminated tuff, cherty tuff, and volcanic wacke; intertonguing calcareous tuff and impure marble are present locally.
The middle unit of the Wassat formation contains coarse-grained clastic beds that suggest a high-energy en vironment. However, the middle unit also contains inter calated marble and tuff units that indicate accumulation in a lower energy subaqueous environment. In the higher beds of the middle unit and in the upper unit, more abundant, thinly laminated beds, as well as some pyritic beds, suggest depo sition under progressively lower energy conditions, possibly in a deepening basin. These transitions form a logical sequence in sedimentation and reinforce the conclusion that the uppermost beds in the Wassat formation are in the eastern part of the outcrop zone.
The final sedimentation phase of the Wassat formation was deposition of the principal sulfide-bearing beds and associ ated thinly laminated tuffaceous and calcareous rocks. Dur ing this phase, little clastic material was furnished to the basin of accumulation, and iron sulfides were deposited from solutions of volcanogenic origin. The sulfur in these sul- fides is characterized by large negative 6 34S values, indicating deposition in a euxinic environment (R.O. Rye, written commun., 1978).
Duwayr formation
The Duwayr formation (Jackaman, 1972) comprises flows of andesite, basaltic andesite, basalt, and rhyodacite, inter- layered with minor andesitic pyroclastic rocks and wacke.
Jackaman reported that the volcanic flows are mostly basaltic andesite in composition, which he plotted in the alkali olivine basalt field of Kuno (1966); these flows range from one meter to as much as 300 m in thickness and commonly show well-developed flow structures. Jackaman suggested that these flows accumulated partly in a subaerial environment; however, the widespread distribution of associated well- bedded sedimentary wacke indicates that much of the depo sition took place subaqueously.
Intrusive rocks
The sedimentary and volcanic rocks in the Wadi Wassat area are truncated both on the north and south by plutonic rocks that range in composition from gabbro to granite. In addition, numerous dikes obliquely transect the rocks of the district (Overstreet and Rossman, 1970; Jackaman, 1972). The oldest intrusive rock is diorite, which is associated with gabbro and granodiorite, followed by biotite granite and a variety of dikes.
The diorite is a fine- to medium-grained, dark-gray rock
8
that locally grades into gabbro and granodiorite. It con tains biotite and locally contains hornblende; in places it is distinctly foliated. Along contacts with metavolcanic and metasedimentary rocks, a hornfels or tactite zone, 10-50 m wide, has developed; pyrite along the contact is locally converted to pyrrhotite. The diorite weathers to smooth slopes with poorly exposed outcrops.
The biotite granite is medium to coarse grained, massive, and equigranular. Near the granite, the calcareous beds were metamorphosed to garnet-diopside rock, and the andesite to biotite schist and hornfels. The granite weathers to promi nent spheroidal boulders characterized by caves, spires, and bridges.
Dike rocks
Many kinds of dike rocks have been mapped in the Wadi Wassat area. Only the more abundant types will be mentioned here.
Diorite dikes occur along the margins of diorite plutons in the northwestern part of the district. These dikes are cut by granodiorite and granite dikes that strike northwest, north-northwest, and northeast, and by felsite (rhyolite?) dikes that mostly strike north.
The rhyolite dikes and the older dikes are cut by younger diabase dikes that mostly trend northwest, but also trend north and northeast. Northwest-trending syenite porphyry dikes were reported by Overstreet (1966d) in the northern part of the area. Diabase dikes are abundant throughout the area mapped on the plate.
Alluvium
Deposits of Quaternary alluvium in the area include eolian silt, sand, and gravel on pediments and wadi floors. The gravel and sand are mostly unconsolidated, but in places they are cemented by secondary iron oxides and caliche and form a crust that is mapped separately. Talus deposits man tle some slopes, especially those below prominent exposures of dikes and silicified rock associated with gossans.
STRUCTURE
The Wadi Wassat iron sulfide deposits are in a north- trending belt of rocks that has been intruded by granitic rocks and complexly folded and faulted. Two kinds of folds have been mapped, major folds and minor folds superimposed on
9
the major folds. The major folds are best delineated by iron sulfide lenses that outline the folds and can be easily traced. Those mapped in the Wadi Wassat area average about 300 m in amplitude.
For convenient description, the sulfide bodies in the map area were divided into four segments (fig. 2). At the northern end of the mapped area, the iron sulfide deposit is truncated by granite. The deposit then extends southward for 8 km (segment I), and turns abruptly in a northwest direction for about 3 km (segment II); thereafter, it turns sharply to the south again for 2.5 km; then it continues to the west for 2 km (segment IV) and butts into granite. These segments were further subdivided into areas (A through K) for purposes of discussion and resource calculations (appendix 1).
Segment I strikes north and generally dips east, 60°-85°, though local overturns were noted. The gossan is nearly con tinuous over this entire segment except for a 1-km gap be tween Areas D and E. At Area E the gossan is exceptionally wide (560 m). This great width is apparently caused by tight parallel folds (fig. 3). Continuing south, past drill hole WS-6, the iron sulfide unit crops out in two parallel belts that may represent two layers or a single folded layer. At the southern end of the segment, the strata turn to strike east-west, then are offset by a north-trending, right-lateral fault. The east-west turn may be a result of drag on the fault or possibly part of an anticlinal fold (fig. 3). In order to clarify these structural features, segment I should be mapped in greater detail.
Segment II strikes northwest and dips mostly to the southwest, though interruptions in the iron sulfide bed suggest local complications due to folding and faulting. Much of the ore zone in this area is covered by alluvium and iron oxide crust, and the details of folding and faulting were not worked out. East of drill hole WS-9, cherty and tuffaceous beds strike northeast, and their dip is steep to vertical; this structure implies a local cross fold. South of drill hole WS-9, calcareous beds overlying the iron sulfide unit form a broad synclinal fold on which are superposed minor folds and lineations that plunge 20°-45°. Though the gossan unit at drill hole WS-9 is interrupted by diorite, it appears to lie in a parallel synclinal fold.
Segment III continues south as a series of lenses, inter rupted locally by granitic bodies and alluvial cover. The lenticularity may be partly a result of folding and partly due to original deposition in lens-shaped bodies. In the wide gap betweeen segments III and IV, the sulfide-bearing zone appears to grade into a cherty tuff unit containing dis seminated pyrite. This unit has an iron-stained surface
10
SA(IR)-372EXPLANATION
Alluvium
r Granitic rocks, rhyolitic (r)
Diorite
Duwayr Formation
-g Wassat Formation, gossan (g)
Con tact dotted wh^re concealed F&ult-dashed where approximately
located; dotted where concealed Fold axis dashed where approximately
located; dotted where concealed, queried where doubtful
Plunge of minor fold Anticline
Syncline
Strike and dip of bedding
Vertical bedding
Overturned bedding
Drill hole
Figure 3.- Detailed map showing structure in the vicinity of drill holes WS-6, -7, and -8.
11
exposure that gives way at a depth of a few centimeters to pyrite disseminations in the cherty host rock.
The iron sulfide unit in Segment IV is intricately broken by intrusive bodies and furnishes little structural information. In several places, however, upright dips to the south were recorded; these are consistent with observations of stratigraphic tops elsewhere in the mapped area.
The folds in the Wadi Wassat area show two major patterns. The right-lateral sense of the large folds in segment I near drill hole WS-7 is consistent with right- lateral movement on north-trending faults of regional extent (Overstreet, 1968<l; Greenwood, 1980). The fold(?)-fault intersection at the southern termination of Area G may have been caused by similar forces.
The broad synclinal fold near drill hole WS-9 lies in a distinctly different setting. The core of the fold contains diorite and granite, and the gossan zone is separated from beds to the north by a postulated fault zone. Some faults in this area were thought by Overstreet (1960ci) to be thrusts formed during the emplacement of intrusive rocks; however, he did not show any thrusts on his geologic map. Jackaman (1972) and Greenwood (1980) advanced similar suggestions. Roberts mapped the area in some detail; his map shows a clear-cut arcuate break between two blocks of contrasting structure (fig. 4). A reasonable structural interpretation of this complex knot is that the two blocks are separated by a thrust fault that dips south at a low angle. Much of the thrust zone is now occupied by dioritic and granitic rocks. These rocks occupy the greater part of the syncline and their emplacement is considered to be the principal force in development of the syncline and associated thrust fault.
In order to completely understand the structure of this block, it should be mapped at a much larger scale so that all significant structural features can be plotted and evaluated.
IRON SULFIDE DEPOSITS
Introduction
Iron sulfide deposits in Wadi Wassat occur in a sedimentary sequence in the upper part of the Wassat formation. This sedimentary sequence includes laminated volcanic ash, cherty tuff, and calcareous slate and tuff. This sequence is as much as 300 m thick but locally pinches out completely along strike. The iron sulfides, mainly pyrite, pyrrhotite, and marcasite, are disseminated throughout the beds and locally form massive lenses along bedding. In places, chalcopyrite and sphalerite grains are scattered sparsely throughout the iron sulfides.
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Pyrite is the principal sulfide mineral at Wadi Wassat (Overstreet and Rossman, 1970; Jackaman, 1972). It occurs in four generations; three of these are primary, and the last is supergene: I, early cubic to anhedral pyrite that occurs mainly along bedding; II, later coarse-grained pyrite that occurs as metacrysts in pyrrhotite; III, veinlets of late pyrite that cut pyrites I and II; and IV, supergene pyrite associated with marcasite in the oxide zone.
The earliest primary pyrite is present as euhedral to anhedral grains and forms layers that commonly are parallel with laminations in the tuff (fig. 5A) . Jackaman (1972) showed that this pyrite mimics bedding and graded bedding. Most grains are equidimensional and range from 50 to as much as 600 microns in diameter (fig. 5B); a few are elon gate due to postdepositional shearing.
Pyrite of generation II formed as metacrysts in pyrrho tite; the most characteristic habit is large cubic crystals as much as 1 cm in diameter. These crystals show skeletal growth on their margins and have replaced the pyrrhotite (fig. 5C) . Pyrrhotite is a metamorphic facies of pyrite that is best developed in zones of contact metamorphism. The pyrrhotite is present as anhedral grains that have rag ged boundaries in contact with silicate gangue minerals.
The youngest primary pyrite (III) is present in frac ture zones and veinlets that cut the older pyrrhotite and pyrite. It is commonly anhedral and is associated with quartz and other gangue minerals (fig. 5D) .
The supergene pyrite (IV) and associated marcasite are mostly fine grained; they are present as concretionary masses and as disseminations in clay in the oxidized zone.
Gangue minerals in the iron sulfide bodies include chloritoid, sericite, biotite, tremolite, quartz, carbonate minerals, epidote, and zoisite. These commonly have re placed the pyrite along grain contacts, indicating that the pyrite developed prior to metamorphism.
The sulfide-bearing bodies at Wadi Wassat are lenticular, and they pinch and swell along strike. In the northern part of the mineralized zone (Segment I, fig. 2), the principal lens is about 3.3 km long and as much as 130 m thick. It consists of interlayered sulfide and silicate layers, as indicated in the logs of drill holes WS-1, -5, -3, and -4 (tables 3, 5, 8, and 10). Holes WS-3 and -4 intersected about 52 m of the ore zone that contains 80 percent or more of sulfide-bearing material.
14
In the southern part of segment I the sulfide zone is as much as 560 m wide; this unusual width is thought to be a re sult of duplication on three or more parallel folds (fig. 3). In drill hole WS-7 (table 13), a cumulative thickness of 52 m contained 80 percent or more of sulfide-bearing material, the same thickness reported for drill holes WS-3 and -4. South of drill hole WS-7 the gossan belt gradually narrows and is less than 100 m wide at the southern end of segment I.
In segment II (fig. 2) the ore zone is poorly exposed. It has a maximum outcrop width of 300 m; however, it is com plexly broken by intrusive bodies and faults and may also be folded, so its true width is uncertain. In drill hole WS-8 (table 17) , about 107 m of sulfide-bearing material were intersected, of which 41 m contained more than 80 percent pyrite and pyrrhotite. Drill hole WS-9 (table 20) cut two sulfide-bearing zones containing a cumulative thickness of 16 m of 80 percent sulfide-bearing material, mostly pyrrhotite.
In segment III the ore zone is narrow, commonly less than 50 m wide, and discontinuous. In segment IV the zone is as much as 250 m wide, but is complexly cut by dioritic and granitic bodies and terminates against granite at its southern end .
Origin of the deposits at Wadi Wassat
The gossans of the iron sulfide deposits at Wadi Wassat were originally interpreted by Overstreet (1968<y p. 6), on the basis of anomalously high molybdenum content, to "have formed from high-temperature sulfide minerals, probably pyrite and pyrrhotite." Later, after a study of core samples from drill hole WS-1, Overstreet and others (196^a) concluded that the pyrite was of mixed sedimentary and replacement origin. Still later, Overstreet (196^6, p. 18) suggested that "the pyrite...was deposited as a hydrothermal re- placement mineral." Overstreet and others tl c/bj£s p. noted that "certain relict textures appear to be of syn- genetic sedimentary or sedimentary-volcanic origin... the Wadi Wassat massive sulfide deposit is obviously poly- genetic..." Overstreet and Rossman (1970, p. 51) reiterated "the concept of a metamorphosed syngenetic deposit... in and partly replacing a... sequence of sedimentary rocks of an- desitic composition and associated bedded volcanic rocks in the andesite sequence."
This concept of a metamorphosed syngenetic deposit was generally accepted by Jackaman (1972), with some modifi cations. Jackaman noted that the pyrite grains mimicked bedding structures such as layering and grading. He
15
SA(IR)-372
Figure 5.- Photographs and photomicrographs of sulfide ore.A. Photograph showing layering in sulfide ore; dark layers are sulfides. B. Photomicrograph of early layered pyrite (p); light-colored layers are quartz
and silicate minerals.16
SA(IR)-372
Figure 5.- Continued.C. Photomicrograph of metamorphosed pyrite and pyrrhotite: pyrite
metacrysts (p) have developed in a matrix of pyrrhotite (po) D. Latest pyrite (p) in veins that cut earlier sulfide and silicate minerals.
17
pointed out that in part the pyrite enclosed original gangue material during growth and in part replaced the gangue. To explain this relationship, Jackaman postulated that the iron and base metals were derived from volcanic exhalations; the metals were thought to have been originally deposited as particles of oxides or hydroxides, then later sulfidized.
We argue that the sulfurization mechanism of Jackaman is improbable. The deposits are in fine-grained rocks that were probably deposited in a shallow to moderately deep aqueous environment (Goodwin, 1973); such rocks would have low permeability, thus inhibiting interstratal movement of solutions. If sulfurization had occurred, it seems likely that some remnants showing stages in the conversion process of oxides to sulfides would have remained. Such remnants have not been reported; therefore Roberts suggests that the iron sulfides were deposited mostly as syngenetic pyrite simultaneous with the deposition of associated siliceous sediments and tuffs. This suggestion is reinforced by the strongly negative sulfur isotope values in the pyrite (R.O. Rye, written commun., 1978)
Overstreet and others (1976, p. 104) considered the gen esis of the deposits from the viewpoint of their geochemis try. They determined the abundances of minor elements in sulfides from the core of drill holes WS-6 and -7 and found that (p. 104) "minor elements in the core... correlate posi tively with syngenetic sedimentary and volcanic deposits and negatively with deposits of hydrothermal, magmatic, and metamorphic origin... the deposit is here thought to be formed under marine volcanic-sedimentary conditions. 11
In view of the emphasis on replacement of groundmass minerals and rock fragments by pyrite (Overstreet and Rossman, 1970; Jackaman, 1972), it seems likely that the formation of the deposits involved more than simple sedimentary processes. The replacement could have been partly a diagenetic process, that is, recrystallization of constituents already present in the rock; it may also have included significant addition of iron sulfides from deep-seated sources, such as visualized by Roberts (1976) for sulfide deposits of dual origin, that is, dual syngenetic and epigenetic deposits found elsewhere in Saudi Arabia. The iron sulfides could have been derived from deep-seated igneous or fumarolic sources that continued to supply metals to the system long after burial .
The essential steps in the formation of the iron sulfide deposits at Wadi Wassat are visualized as follows:
1. Volcanism and sedimentation resulted in the accumu lation of pyroclastic, sedimentary, and volcanic rocks.
18
Fine-grained, massive syngenetic pyrite was deposited in layers and pods during periods of slow accumulation of volcanic and clastic materials.
Analyses of sulfur isotope ratios in sulfides from Wadi Wassat by Rye and others (1979) show strongly negative
values (-15.3 to -30.5 permil), which indicate de position in a euxinic environment. The sulfur is considered by Rye to be largely derived from sea water sulfates.
2. Diagenetic alteration, including zeolitization, cem entation and other processes, of the pyroclastic and sedimen tary rocks followed. Some rearrangement of the iron sulfides probably took place at this time, leading to recrystal- lization and coarsening in grain size of the iron sulfides.
3. Possible late-stage introduction of iron sulfides and minor amounts of base metal sulfides from fluids of deep- seated (volcanogenic) origin also may have taken place (Corliss, 1971; Anderson and Halunen, 1974; McMurty and Burnett, 1975). Mauger (1972) has suggested that metals and sulfur in such deposits may be extracted from sediments by pore waters during compaction; the metal-bearing waters may move upward and deposit sulfides around submarine spring vents. Wright (1965) has also discussed the movement of metals through volcanic rocks.
4. Regional metamorphism and recrystallization of the rocks followed, favoring an increase in grain size of the pyrite and segregation into layers.
5. Finally, intrusion of diorite and granite bodies caused deformation, further recrystallization of pyrite to pyrrhotite , and mobilization of sulfides on a small scale.
Sampling program
In 1967 Rossman supervised the collection of about 1,200 gossan samples, of which 272 were analyzed in the USGS-DGMR Chemical Laboratory. The results of these analyses are sum marized in table 1.
In March and April 1975, the cores of drill holes WS-1 through WS-9 were resampled at 1-m intervals and reanalyzed. Also, about 450 surface samples were collected for comparison of the geochemistry of surface samples with those from the cores (appendices 1 and 2). Most of the samples have been analyzed for manganese, nickel, cobalt, copper, lead, zinc, silver, gold, molybdenum, and chromium to facilitate direct comparison of the results with samples from Wadi Qatan (Dodge and Rossman, 1975).
19
Tabl
e 1. Su
mmar
y of
analytical
rcr,
ults
fr
om ;?
?,^
00:^-1*:,
rawp
ler,
, WaAi.
Vac sa
t[G
ossa
ns d
esignated
by le
tter
s, as a
n plate
1.
All
'results in
pa
rts
per mi
llio
n except silver-,
vdiich is
expressed in
oun
ces
[x?r
to
n.
Copper,
molybdenum,
and
x.in
c we
re a
naly
sed
chem
ical
ly,
silv
er
by ato
mic
absorption,
nickel a
nd c
obalt
by semiquantitative sp
ectr
ogra
phy.
-, in
dica
tes
not
anal
yzed
]
to o
Mean
High
Mean
Hi
gh
Valu
es
Mean
High
Mean
Hi
gh
Mean
High
Cu 25
115 10
10 10 18
60 37
150 24
150
Mo Gossan
4 40 Gossan
35
75 Gossan
15 Gossan
4 10 Gossan
11
40 Gossan
6 20
Zn L 30
22
50
Ag
Ni
samples
0 10
0
10
Co 10
10
K 3 sa
mple
s
16
250
10
0 10
10
10
J 1 sa
mple
25 I (SE
15
50 H 15
15
50
G--25
8 25
0 10
part) 5
samples
.04
.19
samp
les
.04
.09
samples
.01
.05
10 - - -
CuMo
Zn
Goss
an E
11
1
Mean
High
Mean
High
Mean
Hi
gh
Mean
Hi
gh
Mean
High
25
225 35
75 6 20 14
30 35
75
10
21
50
100
Goss
an
5 10
Goss
an
D--4
25
25
Ag
samples
.04
.04
samples
-
Ni 10
10 10
10
Co 10
10 10
10
C 16
samples
5 25
- 10
50
Gossan
7 115 Go
ssan
14
40
10
1010
10
B 25
samples
6 25 A 4
12
25
- samples
-
10
10 10
10
10
10 10
10
Bedded a
ndesitic tuff 11 samples
Mean
Hi
gh30
60
5 2025
25
-10
10
10
10
Mean
12
Goss
an F
(W part) 22 s
amples
5 5
.04
Description of the deposits
The gossans of iron sulfide deposits in Wadi Wassat are discontinuously exposed along a sinuous zone having a total strike length of about 16 km and a width of as much as 300 m. The lack of continuity is due in part to faulting, in part to folding, and in part to alluvial cover. The depth of oxida tion in the district is variable, ranging from 16 m to 30 m.
Table 2. Depth of oxidation in the areaVertical depth
Drill hole Comment (in meters)
WS-1 Depth to sulfides 20WS-4 Depth to fresh bedded rock 16WS-6 Depth to massive sulfides 23WS-7 Depth to massive sulfides 17WS-8 Depth to unweathered bedded rock 17WS-9 Depth to fresh andesitic rock in
flank of hill 30
The gossans will be described, beginning in the northern part of the area and continuing to the southwestern part (see plate). Areas of outcrop, as designated on figure 2, will be described separately as areas A to L, together with tables of descriptions and analyses of drill cores.
Area A Gossan
Area A gossan (17,520 sq m), in the northern part of the area (see plate), is about 720 m long and as much as 90 m wide. The area was sampled along several lines, and two dia mond drill holes, WS-1 and WS-5, were put down in the gossan. The results of assays of surface samples are given in appendix 1.
Drill hole WS-1.--Hole WS-1 is located near the northern end of the mapped area, at an altitude of 1,203 m (see plate). It was drilled S.67°E., at an inclination of -45°, and is 139.5 m long. Fresh sulfides were encountered at a depth of 30 m, where a mineralized zone 68 m thick was inter sected (table 3). This zone contained a cumulative thickness of 25 m of 80-100 percent iron sulfide-bearing material (fig. 6A) .
21
SA(IR)-372WS-1
EXPLANATIONWS-5
1200 METERS
Alluvium
Gossan
Zone number | |- 10-50'w
50-80
80-100
Percent suitide in core
100 METERS
153.6 meters
B. Section facing North
139.5 meters
WS-3
A. Section facing N.20°E.
WS41200 METERS-
129.9 meters
C. Section facing N.10°W.
Figure 6.- Cross sections along drill holes WS-1, -5, -3, -4, -6, -7, -8, and -9.
22
WS-6
SA(lR)-372
WS-7
1200 METERS
D. Section facing N.23°E.
WS-8
1 52.6 meters
F. Section facing N.45°W.
138.5 meter*
E. Section facingN.25°E.
WS-9
1200 METERS
154.4 meters
G. Saction facing N.15° E.
Figure 6.- Continued.
23
Table 3 .--Summary log of drill hole WS-1[Percent pyrite shown in parentheses]
Interval (meters) Description
0-30 Oxidized material30-31 Massive pyrite31-43 (80)43-47 Andesite bedded sequence (10)47-58 Diorite (10)
58-75 Fine-grained diorite75-76 Andesite bedded sequence76-78 15 percent pyrite grading to 30
percent pyrite at 78 m78-80 Andesite, well-bedded (20)80-83 (40)
83-85 (30-40)85-86 (10-15)86-87 (50)87-89 (60-80)89-90 (80)
90-92 (90)92-93 (20)93-95 75 percent pyrite (6 to 12 cm
intervals of 20 percent pyrite) 95-101 (90) 101-103 Fine-grained bedded andesite
103-107 (90)107-108 (50-75)108-110 (30) well-bedded110-111 (5-25)111-113 (20-30)
113-122 Fine-grained bedded andesite122-132 Fine-grained bedded andesite132-139.5 Fine-grained bedded andesite, end of
hole
24
An electromagnetic survey by Alien and Davis (196^a, b) showed a pronounced high east of the projected end of hole WS-1. Hole WS-5 was drilled to test this magnetically high area and intersected 6.72 m of massive sulfides.
Analyses of core samples from hole WS-1 are given in table 4.
Drill hole WS-5.--Hole WS-5 is located about about 100 m east of hole WS-1, at an altitude of 1,201 m. It was drilled S.72°E., at an inclination of -60°, and is 103 m long (table 5). Hole WS-5 was designed to intersect a mineralized zone and an electromagnetic anomaly east of the zone explored in hole WS-1 (Alien and Davis, 196%, b) . The hole passed through bedded andesitic tuff and intersected massive pyrite and pyrrhotite at 53 m. A cumulative thickness of about 7 m of 80 percent iron sulfide-bearing material was found (fig. 6A) .
Analyses of core samples from hole WS-5 are listed in table 8, and major element chemical analyses are in table 7.
Area B gossan
Area B (105,110 sq m) is 1700 m long and as much as 200 m wide; it is displaced about 500 m to the southeast from area A along a northwest-trending, left-lateral fault. The gossan is siliceous and crops out as a prominent ridge for most of this distance; at the southern end it has been cut by many dikes of granitic to granodioritic composition. The results of surface sampling are given in appendix 1.
Three holes, WS-2, -3, and -4, were drilled in area B. Hole WS-2 was in rubbly rock that caved in; the hole was accordingly abandoned. The summary logs and analyses of the core of holes WS-3 and WS-4 follow (tables 8-12).
Drill hole WS-3. Hole WS-3 is located 200 m southeast of hole WS-2, at an altitude of 1,215 m (see plate). The hole was drilled west, at an inclination of -45°, and is 158.6 m long. Eighty meters of mineralized rock were intersected , of which about 52 m contained 80 percent or more sulfide-bearing material (fig. 6B, table 8).
Drill hole WS-3 intersected massive sulfides at a depth of 46.5 m and remained in sulfide-bearing material to a depth of 132 m. This sulfide-bearing interval appears to be repre sentative of the Wadi Wassat sulfide deposits; it consists of marginal zones of massive pyrite and a central zone contain ing 10-50 percent pyrite. Analyses of core samples are given in table 9.
25
Table 4 .--Analyses of cores from drill hole WS-1[Material analyzed: MP, masive pyrite; DP, disseminated pyrite. Copper, results in parts per million, determined by semiquantitative spectrography by C.E. Thompson, USGS, and Mohamed Jambi, DGMR. Gold and silver, results in ounces per ton, determined by fire assay by S,M. Bahijrij DGMR. tr = trace, nil = not detected, -= not analyzed]
Sample number
3101031011310283101231029
3101331030310143101531031
3101631017310183103231019
3103331020310343102131035
3102231036310233102431037
310253102631027
Interval (meters)
29-3032-34
3536-38
39
4041427678
7982858688
8991939496
9799
100104105
106109112
Copper
1010101070
1010702070
2030201020
1015701010
1010010 15
____
Gold
trtr.02trtr
trnilnilnil
0.02
trnilniltrnil
trniltrtrtr
nil.02nil.02.02
nilnilnil
Silver
0.26.49nil1.68.12
.38
.14
.52
.16nil
.8nil
1.04nil.52
nil.12nil.46nil
.35nil.54.6.12
.92
.82
.88
Material analyzed
MPMPMPMPDP
MPDPMPMPDP
DPDPDPMPDP
MPMPDPMPMP
MPDPMPMPMP
MPDPDP
26
Table 5. Summary log of dr-lll hole WS-5[Percent pyrite shown in parentheses]
Interval (meters)
0-50 50-5353-5454-5555-57
57-59 59-63 63-6565-6666-67
67-6868-6969-7070-73 73-76
76-79 79-83 83-8989-9090-103
Description
Bedded andesite Andesite Pyrite (60) Pyrite (85) Pyrite (40)
Pyrite (30-50) Pyrite, mainly Gray andesite, Gray andesite, Pyrite (60)
pyrite (10)
in veins (30) pyrite (10) pyrite (20)
Black bedded rock (10) Gray andesite Black bedded rock (10) Pyrrhotite (10) Pyrrhotite (90)
Pyrrhotite-pyrite (20-50) Pyrite-pyrrhotite (90) Pyrite-pyrrhotite (10) Pyrrhotite-pyrite (10) Gray andesite, end of hole
27
Table 6. Analyses of core from drill hole WS-5
[Copper results in ppm, silver and gold in ounces per ton, percent pyrite in parentheses. Chemical analyses by Ibrahim Baradja, fire assays by S.M. Bahijri, and semiquantitative spectrographic analyses by Mohamed Jambi, USGS-DGMR Chemical Laboratory]
Sample number
35095
35094
35093
35092
35091
35090
35089
35088
35087
35086
35085
35084
35083
35082
35081
Interval (meters)
52
54
56
59
61
63
66
68
70
74
76
79
81
83
86
CopperSpectro- Chemical graphic
50
15
15
20
20
50
20
30
20
30
20
15
10
70
30
15
<10
15
30
40
75
30
40
20
30
10
<10
<10
115
60
GoldFire
nil
nil
nil
nil
nil
nil
nil
nil
nil
nil
nil
nil
nil
nil
nil
Silverassay
0.14
nil
.12
.26
.48
.46
.52
.09
.62
.26
.44
.13
.14
.13
.18
Material analyzed
Andesite
Pyrite (60)
Pyrite (40)
Pyrite (30)
Pyrite (30)
Pyrite (30)
Pyrite (30)
Andesite
Pyrite (10)
Pyrite (90)
Pyrite( 20-50)
Pyrite (90)
Pyrite (90)
Pyrite (10)
28
Table 7. Ma
jor
element
chemical an
alys
es of
core from d
rill
ho
le WS-5
[*,
indicates
total
S an
d Fe,
resp
ecti
vely
. Ra
pid
rock
ana
lyse
s un
der
the
dire
ctio
n of L.
Shapiro, USGS L
aboratory, Wa
shin
gton
, D.
C.]
Samp
le
numb
er
35095
35094
35093
35092
35091
3509
035
089
3508
8CD
35087
35086
35085
35084
3508
33508
235
081
Interval
(meters)
52 54 56 59 61 63 66 68 70 74 76 79 81 83 86
Si0
2
20.2
12.5
35.2
41.9
54.1
46.1
48.4
40.7
39.0
18.1
49.9
17.8
16.5
45.6
49.4
A120
3
6.2
3.1
9.9
12.0
14.2
11.4
13.4 9.3
9.1
3.1
5.4
1.1
1.8
11.7 7.7
S* 30.1
37.8
22.1
16.5 9.0
13.3 7.5
15.8
18.2
16.2
15.5
36.1
32.7 9.6
6.2
Fe*
30.1
35.7
21.9
17.1
10.6
17.9
11.1
23.1
22.5
44.2
19.8
35.9
32.5
14.8
16.8
MgO
1.6
1.0 .85
1.0
1.5
1.5
2.3
1.0 .90
.25
.50
.37
.45
3.4
4.6
CaO
r&20
K20
(Res
ults
in weight
2.8
1.8
1.2
1.7
1.0 .55
2.6
1.4 .25
.45
2.7
1.0
6.4
3.0
4.6
0 0 1.2
2.1
2.5 .15
.75
0 .45
0 0 0 .15
1.2 0
1.9 .45
2.2
2.2
2.0
2.0
2.4 .85
1.2 .60
.20
.20
.25
2.5 .44
H20-
H2CH-
perc
ent)
0.61 .69
.44
.31
.33
.37
.68
.27
.46
.58
.58
.27
.21
.29
.61
1.8
3.2
1.8
1.8
2.7
1.6
4.2
4.0
3.4
1.7
2.4
1.8
2.0
3.4
3.9
Ti0
2
0.49 .14
.44
.47
.58
.54
.70
.46
.25
.19
.40
.20
.18
.48
.67
P20
5
0.22 .18
.16
.17
.17
.19
.21
.19
.22
.25
.16
.17
.17
.38
.30
Nfri
O
0.08 .14
.04
.05
.06
.10
.13
.08
.07
.09
.09
.03
.04
.13
.15
002
0.30 .94
.05
.42
.05
.08
2.8 .69
.45
1.2 .21
.62
2.9 .68
.58
Sum 96 98 97 97 99 96 97 98 96 87 98 96 96 97 91
Table 8. Summary log of drill hole WS-3 [Percent pyrite in parentheses]
Interval (meters) Description
0-29 Porphyritic syenite dike29-38 Weathered andesite38-39.5 Disseminated pyrite in andesite
39.5-46.5 Andesite46.5-61 (90)
61-61.5 (10)61.5-62 (80)
62-64 (20-30)64-66 (90)66-67 (85)
67-68 (20)68-86 (90)86-90 (50)90-93 (75)93-94 (50)
94-95 (15)95-96 Core missing96-100 (10-25)100-103 Andesite (25)103-111 (90)
111-118 (80)118-119 (10)119-121 (70-85)U'l-122 (10)122-123 Bedded andesite
123-123.5 (20)123.5-124 (30)126-127 (20)127-129 (40)132-143 Andesite
143-153.6 Brecciated andesite, no sulfidesend of hole
30
Table 9. Analyses of core from drill hole WS-3
[n.d. = not determined; - = not found; tr = trace. Gold and silver determined by fire assay by S.M. Bahijri. Copper of samples 31038, 31039, and 31040 determined by semiquantitative spectrographic analysis by C.E. Thompson and Mohamed Jambi. All other copper, lead, and zinc determinations are colorimetric chemical analyses by Saeed Osman. Work done at USGS-DGMR Chemical Laboratory]
Sample Number
3103831039310403911339114
3912339124391253912639120
3912139122391183911939131
3913239133391273912839129
Interval (meters)
48-4953-5456-586166
6972757880
84879093103
108110111114116
Gold Silver Copperounces per ton
tr 0.12 0.0015tr .11 .0015tr .23 .0015
<.002< .002
<.002_ _ _
< .002<.002< .002
< .002<.002< .002.005
< .002
< .002<.002< .002
n .d . - .002.002
Leadpercent
n.d.
<.0025<.0025
<.0025_
< .0025<.0025<.0025
<.0025<.0025< .0025<.0025< .0025
< .0025<.0025<.0025<.0025<.0025
Zinc
_
<.005<.005
<.005
.005
.005<.005
<.005<.005<.005<.005<,005
<.005<.005<.005.015.005
39130 121
31
Drill hole WS-4. Hole WS-4 is located about 700 m south east of hole WS-1 (see plate), on the western side of the gossan explored by holes WS-2 and -3. The collar of the hole is at an altitude of 1,200 m. The hole was drilled N.80°E., at an inclination of -45°, and is 129.9 m long. It was in mineralized rock for 77 m, of which about 52 m contained 80 percent or more sulfide-bearing rock (fig. 6C) .
The hole was drilled to intersect the sulfide zone be neath a gossan. Although massive pyrite was intersected at a depth of 28 m, the principal body was not cut until 42 m (fig. 5C, plate). The hole probably passed through most of the mineralized zone (table 10). Massive pyrite is present both above and below the steeply dipping zone, with 5 to 50 percent pyrite in the center. Analyses of core samples are given in table 11. Major element chemical analyses are given in table 12.
Area C
Area C covers an area of 19,880 sq m and contains gossan outcrops over a strike length of about 780 m and a width of as much as 65 m. It overlaps slightly with area B, sugges ting either that it is a separate mineralized lens or a segment displaced on a north-northwest-trending, right- lateral fault.
Area C was sampled along several lines. Assays of gossan surface samples are given in appendix 1.
Area D
Area D covers an area of 24,240 sq m and is 650 m long am; us much as 60 m wide. It is a continuation of area C, bu has been displaced about 100 m to the east on a northwest-trending, left-lateral fault. At the southern end, the gossan either pinches out completely or plunges beneath the surface.
Assays of gossan surface samples are given in appendix 1.
Area E
Area E covers an area of 289,780 sq m and is 2.1 km long and as much as 560 m wide. This unusual width may be the re sult of duplication by folding and the mineralized zone may also be thicker here. Several mineralized beds may be present; some units on the western side are siliceous and crop out prominently. The units on the eastern side are not resistant and are overlain in places by soil crustified with iron oxides, sulfur, melanterite, and other secondary minerals.
32
Table 10. Summary log of drill hole WS-4[Percent pyrite shown in parentheses]
Interval (meters) Description
0-13 Weathered andesite13-23 Gray andesite23-28 Weathered andesite28-29 (80)29-30 Core is soft, weathered, and contains
veinlets of melanterite30-31 Oxidized material31-32 (90)32-34 (90); lower 3.6 cm contains
disseminated pyrite34-35 Andesite (10)35-39 Disseminated pyrite in calcite39-56 (90)56-58 (30-50) with calcite58-59 (50-75)59-60 (30)60-61 (80)61-62 (30)62-64 (10)64-66 (10-20)66-75 Pyritiferous bedded andesite75-76 (90)76-76.5 (15)
76.5-77 (30-40)77-78 (80)78-80 (20)80-81 (10)81-81.5 (75)
81.5-83.5 (30-40)83.5-84 (50)
84-85 (10)85-87 (20-30)87-91 (90)91-92 90 percent pyrite and pyrrhotite92-93 (20-40)93-94 (90)94-95 (10-30)95-105 90 percent pyrite except for 0.3 m
bedded interval at 101 (30 percent)105-114 90 percent pyrite except for 0.5 m
rhyolite dike at 114 m114-117 (90)117-121 (10-40)121-129.9 (10-30), end of hole
33
Table 11. Analyses of core from drill hole WS-4[ tr = trace, nil = not found, - = not determined. Copper results in parts per million, gold and silver in ounces per ton. Material analyzed: MP, massive pyrite; DP, disseminated pyrite; percent pyrite in parentheses. Chemical analyses by I. Baradja, fire assays by S.M. Bahijri, semiquantitative spectrographic analyses by K. Shahwan, USGS-DGMR Chemical Laboratory]
Sample number
3503735038350393504035041
35041A35042350433504435045
3504635047350483504935052
3505435055350563505735058
3505935063350653506835069
3507035071350723507335074
3507635077350783507935080
Interval (meters)
2831343542
4548515054
5558616467
7073767982
8587919399
102105108111114
117120124127125
CopperSpectro- Chemical graphic
1515 <2015 <10
101010 <- <
2040404040
4070301515
1515 <151515
1510101010
1020202030
CIOCIOCIOCIOCIO
CIOCIOCIOCIOCIO
CIO20202010
6075CIO30CIO
(10CIOCIOCIO(10
(10CIO(101010
1010301060
GoldFire
nilnilniltrtr
trtrtr tr
nilnilnilnilnil
nilnilnilnilnil
nilnilnilnilnil
nilnilnilnilnil
nilnilnilnilnil
Silverassay
0.09.09.13.27.17
.21
.18
.26 .26
.17
.34
.28
.32
.36
.09
.16
.05
.21
.05
.08
.06
.12
.15
.14
.52
.15nil.08.06
.11
.18
.13
.16
.34
Material analyzed
MPMPDPDPMP
MPMPMP9
MP
MP(30-50)
(30)9
(1CK30)
(10-20)DPMP(20)
(30-40)
(10)(20-30)
MP(90)(90)
(90)(90)(90)(90)(90)
MP(10-40)(10-30)(10-30)(10-30)
34
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35
Surface samples collected in the area were analyzed (appendix 1).
Drill hole WS-7. Hole WS-7 is located on the northeas tern side of the gossan (see plate). The hole was drilled N.65°W., at an inclination of -45°, for a length of 138.5 m. The altitude at the collar of the hole is 1,225 m. The hole penetrated only a small part of the mineralized zone overlain by gossan. The gossan along the western side of the area was not explored, either by drilling or by geophysical surveys. About 103 m of mineralization were intersected in the hole, of which a cumulative thickness of 52 m contained more than 80 percent sulfide-bearing material (fig. 6E, table 13).
Analyses of core from drill hole WS-7 are given in table 14.
Area F
Area F is a continuation of area E and is located on the southern side of Wadi ab Arram. It consists of two lenses of gossan whose combined area is about 34,910 sq m; the longer lense is 370 m long and as much as 100 m wide, and the shorter lense is about 360 m long and as much as 60 m wide.
Analyses of surface samples are given in appendix 1.
Drill hole WS-6. Drill hole WS-6 was drilled into the into the gossan on the eastern side of area F. The collar is at an altitude of 1,235 m. The hole is 91.5 m long and was drilled S.67°E., at an inclination of -45°. About 26 m of material containing 80 percent or more pyrite-bearing material were cut in the hole (fig. 6D, table 15). Analyses of the core are given in table 16.
Area G gossan
Area G gossan covers an area of 35,600 sq m and is a southward continuation of area F. It has been displaced about 200 m to the southeast of area F on a northwest- trending, left-lateral fault. The gossan ends against another fault that trends north. The gossan is 1,100 m long and as much as 130 m wide. Some parts are siliceous and crop out prominently, but much of the gossanous area has low relief.
The analyses of surface samples are given in appendix 1.
Area H gossan
The gossan of area H is about 1,100 m long and is as much as 320 m wide. It covers an area of 74,580 sq m and strikes
36
Table 13. Summary log of drill hole WS-7[Adapted from Overstreet and others, Percent pyrite in parentheses]
Interval (meters) Description
0-16.416.4-17.217.2-19.719.7-25.224.2-33.0
33.0-33.533.5-42.042.0-42.8
42.8-50.050.0-52.5
AlluviumAplite (1)Altered diorite (1)Gossan and gouge(90-99)
Gypsiferous massive(85-99)Disseminated pyrite
(20-70)(95-99)Disseminated pyrite
(20-60)
pyrite
in argillite
in agglomerate
52.5-71.0 71.0-72.4
72.4-78.8 78.8-83.5 83.5-92.9
92.9-94.8 94.8-108.8 108.8-117.5 117.5-119
119-126.4
126.4-128.5 128.5-138.5
(90-99)Interlayered massive and disseminatedpyrite (40-99)
Disseminated pyrite (20-60) Massive pyrite Disseminated pyrite
Massive pyrite Disseminated pyrite (85) Disseminated pyrite (10-30) Massive pyrite (85-80) Massive and disseminated pyrite,
interlayered (1-15)
Disseminated pyrite (2-5) Massive andesite, disseminated pyrite (0.5), end of hole
37
Table 14. Analyses of core from drill hole WS-7[nil = not detected. Chemical analyses for copper and zinc by John C. Chandler, USGS Laboratory, Washington, D.C. Fire assays for gold and silver by M. Fourati, USGS-DGMR Chemical Laboratory]
Sample number
3008730088300893009030091
3009230093300943009530096
3009730098300993010030101
3010230103301043010530107
3010830109301103011130112
3011330114301153011630117
3011830119301203012130122
Interval (meters)
24-2629-3032-3339-4042-42.5
45-45.547-47.5
48.4-49o & o ~o o54.5-55
58-58.561-61.564-64.567-67.570-70.5
73-73.576-76.579-79.582-82.585-85.5
88-88.591-91.594-94.5
97.5-98100-100.5
103.5-104106.5-107109.5-110112.5-113118.5-119
122-122.5125-125.5128-128.5131-131.5134-134.5
Copper(parts per
10<2<25
37
1071<2<24
7<211<29
282110<224
7414
4572
3793622843
4620717343
Zincmillion)
35
<29
72
3441034276
1616298
37
4751461349
3242213636
3290503524
5129576232
Gold(ounces
nilnilnilnilnil
nilnilnilnilnil
nilnilnilnilnil
nilnilnilnilnil
nilnilnilnilnil
nilnilnilnilnil
nilnilnilnilnil
Silverper ton)
0.48.40.34.47.24
.16
.23
.39
.40
.32
.32
.32
.12
.04
.24
.28
.28
.38
.23nil
nil.06
nilnil.16
nil.06.04
nilnil
.06
.12
.40
.26
.28
30123 137-137.5 56 43 nil .16
38
Table 15. --Summary log of drill hole WS-6
[Adapted from Overstreet and others, 1969 Percent pyrite in parentheses]
Interval Description(meters)___________________________________________
0-18.2 Alluvium and weathered rock18.2-21.2 Gossan21.2-22.7 Leached gray andesite22.7-25.1 Leached microdioritic porphyry25.1-27.3 Leached microdiorite
27.3-30.3 Leached diorite altered togypsiferous rock
30.3-33.3 Clay, gypsum, and iron oxide 33.3-35.7 Upper part of interval is oxidized;
lower part is massive pyrite 35.7-43.3 (95) 43.3-48.0 (90)
48.0-55.7 (95)55.7-58.8 Massive and disseminated pyrite,
average (40)58.8-62.0 (85-90) 62.0-64.0 Average (40) 64.0-66.8 (5-15)
66.8-68.2 Disseminated pyrite in microdiorite(30-60)
68.2-69.2 Andesite with disseminated pyrite 69.2-71.2 Disseminated pyrite in andesitic
agglomerate (5-60) 71.2-74.2 Disseminated pyrite in andesitic
agglomerate, (up to 25) 74.2-91.5 Disseminated pyrite in masssive
andesite and andesitic agglomerate(1-15)
39
Table 16. Analyses of core from drill hole WS-6
[nil = not detected. Copper and zinc results in parts per million, silver and gold in ounces per ton. Chemical analyses for copper and zinc by John C. Chandler, USGS Laboratory, Washington, D.C. Fire assays for gold and silver by M. Fourati, spectrographic analyses for copper, USGS-DGMR Chemical Laboratory]
Sample number
30129
30130
30131
30132
30133
30134
30135
30136
30140
30144
Interval (meters)
48.5-49
51.5-52
54.5-55
57-58.5
60-61.5
64-64.5
67-67.4
70-70.5
79-79.5
88-88.5
Copper Gold Silver ZincChemical Spectro
graphic
5
10
5
5
14
9
68
86
78
60
<10
<10
<10
<10
10
10
75
115
115
75
nil
nil
nil
nil
nil
nil
nil
nil
nil
nil
0.24
.60
.54
.61
.50
.66
.68
.60
.68
.62
27
8
8
14
16
11
22
42
11
12
40
north-northwest and dips west-southwest. Originally the mineralized zone of area H was probably continuous with that of area G, but is now displaced about 400 m to the north of area G. On the north, gossan H apparently ends against a fault in Wadi ab Arram.
Analyses of surface samples collected in area H are given in appendix 1 .
Drill hole WS-8. Hole WS-8, which was drilled in the northwestern part of the gossan, is at an altitude of 1,244 m; it is 152.6 m long and was drilled N.45°E., at an inclina tion of -45°. About 107 m of massive and disseminated pyrite and pyrrhotite were cut in the hole; of this, a cumulative thickness of 41 m is 80 percent or more sulf ide-bearing material (fig. 6F, table 17). Analyses of core samples are tabulated in table 18. Major element chemical analyses of 30 samples from drill hole WS-8 are given in table 19.
Area I gossan
Gossan bodies in Area I cover an area of 76,900 sq m and are scattered along a zone about 1,300 m long and 200 m to 300 m wide. The bodies are poorly exposed and crop out mostly on low hills that rise only a few meters above the pediment surface. At the northwestern end of the area, the mineralized zone forms a tight arc as it bends from a northwest-trending strike and southwest dip to a southwest- trending strike and southeast dip.
Analyses of surface samples are given in appendix 1.
Drill hole WS-9. Hole WS-9 was drilled in the north western part of the gossan. The collar of the hole is at an altitude of 1,265 m; it is 154.4 m long and was drilled N.75°W., at an inclination of -45° (fig. 6G, table 20). It penetrated two sulfide zones about 88 m apart; the cumulative thickness was 16 m of 80 percent sulfide-bearing material, mostly pyrrhotite.
Analyses of core from hole WS-9 are given in tables 21and 22.
41
Table 17. Summary log of drill hole WS-8
IntervalDescription(meters)______________________________________________
0-27 Weathered material27-34 Andesite intruded by granite at 32 m34-38 Gray, fine-grained andesite with
feldspar phenocrysts38-39 30-50 percent pyrite-pyrrhotite39-41 Gray andesite, 90
41-44 80 pyrite44-48 90 pyrite48-49 50 percent pyrite-pyrrhotite49-58 90 percent pyrite-pyrrhotite58-59 75 percent pyrite-pyrrhotite
59-64 80 percent pyrrhotite64-65 Gray andesite (<10 pyrite)65-67 40 percent pyrrhotite67-69 10 percent pyrrhotite69-70 75 percent pyrrhotite
70-82 90 percent pyrrhotite82-84 30 percent pyrrhotite84-85 90 percent pyrrhotite, disseminated
pyrite85-86 50-70 percent pyrrhotite86-87 90 percent pyrrhotite
87-95 Gray andesite, intruded by granite95-96 Andesite96-99 Massive pyrrhotite99-108 Disseminated pyrrhotite108-109 85 percent pyrrhotite
109-110 45 percent pyrrhotite110-112 Massive pyrrhotite112-116 Gray andesite116-117 80-90 percent pyrrhotite117-121 Gray andesite, 30 percent pyrrhotite
121-125 Gray andesite125-134 Gray andesite intruded by diorite134-135 Gray andesite135-136 80-90 percent pyrrhotite136-142 Gray andesite intruded by diorite
142-143 10-50 percent pyrrhotite143-144 Gray andesite, 90 percent pyrrhotite144-152.6 Gray andesite intruded by diorite
except for the interval 149-150 m which is 30-50 percent pyrrhotite, end of hole
42
Table 18. Analyses of core from drill hole WS-8
[- = not determined. Copper results in parts per million, silver in ounces per ton. Material sampled: MP, massive pyrite; DP disseminated pyrite. Percent pyrite in parentheses. Chemical analyses for copper by Ibrahim Baradja, fire assay for silver by S.M. Bahijri, spectrographic analyses for copper by K. Shahwan, USGS-DGMR Chemical Laboratory]
CopperSample number
3512535124351233512235121
3512035119351183511753116
3511535114351133511235111
3511035109351083510735106
3510535104351033510235101
3510035099350983509735096
Interval (meters)
3941434750
5356596164
6670727577
8184858790
94-
112118
121130136142144
SilverSpectro- Chemical graphic
_----
_----
_20202020
2030203070
3015201570
7010010070
100
_----
_----
_10101010
10101010
115
6020101015
7522510-
10
0.14.04.02.10.06
.09
.02
.32
.40
.12
.02
.08
.06
.14nil
.11nil.14.17
1.06
1.12.06.24.36.38
.32
.16
.36
.24
.16
Material analyzed
(90)(90)(90)(90)(90)
(90)(90)(75)(80)(80)
(40)(75)(90)(90)(90)
(90)(30)(90)DP(50-70)
(90) _MP(80-90)
(30)Andes! te(80-90)(60)Andesite
43
Tab
le 10.
Majo
r el
emen
t ch
emic
al
analy
ses
of
coi-
e fr
om
M
S-8
[*
indic
ates
to
tal
S an
d F
e,
resp
ecti
vely
. R
apid
ro
ck a
nal
yse
s un
der
the
dir
ecti
on o
f L
. S
hap
iro
, U
SGS
Lab
ora
tory
, W
ashi
ngto
n,
D.C
.]
Sample
number
3512
535
124
3512
335
122
3512
1
3512
035
119
3511
835117
35116
35115
35114
3511
335112
35111
35110
35109
3510
835
107
35106
3510
535
104
3510
335
102
3510
1
35100
3509
935098
3509
735096
Interval
(met
ers)
39 41 43 47 50 53 56 59 61 64 66 70 72 75 77 81 84 85 87 90 94 - 112
118
121
130
136
142
144
Si0
2A1
203
S*Fe
*%o
CaO
(Results
30.8
33.6
23.2 9.0
24.6
11.7
16.4
44.1
17.2
13.8
46.4
20.7
12.2
18.6
25.7
21.0
15.5
32.6
27.9
39.8
48.7
38.6
20.7
54.6
38.3
43.8
44.4
17.6
23.1 9.4
7.8
10.5 7.4
4.2
5.6
4.4
6.0
14.0 5.5
4.5
14.1 6.3
4.2
5.5
8.3
7.5
4.8
8.8
9.3
12.3
15.5
10.5 8.0
18.2
12.3
12.4
14.7 6.3
6.7
2.8
16.6
12.8
15.7
25.3
15.9
16.8
21.8 9.4
22.8
22.8 7.6
27.2
36.6
26.1
13.8
20.8
19.7
13.4
10.0
12.3 5.6
12.7
24.7 2.2
6.5
7.9
7.7
17.6
20.8
18.2
32.7
29.1
36.6
48.7
40.1
42.4
44.6
16.9
16.8
41.0
15.8
37.3
37.1
39.3
37.8
36.2
39.2
31.6
31.2
16.7 9.4
20.4
35.2 6.6
23.4
15.3
15.5
42.0
37.2
50.4
1.2
1.6
1.4 .35
.92
2.2 .70
2.1
2.2 .80
2.8 .92
1.0 .65
.80
1.0
1.0
1.2
1.1
3.4
4.7
2.4
1.3
2.6
2.4
4.1
2.5 .80
.85
.17
1.2
2.3
4.0
1.4
1.0
6.5
1.3
2.6
3.7
1.5
2.8
1.9
2.0
1.1
1.3
3.2
1.8
1.2
1.6
3.1
4.2
5.0
1.7
4.1
2.1
3.4
2.1
1.9
1.6
1.6
Na.20
K20
H2O-
H2O
in w
eight
perc
ent)
1.4
1.2
0.50
0.90
2.3
1.0
.16
.94
1.2
.85
.18
.80
.45
.40
.52
.38
1.4
1.2
.08
.58
.25
.72
.09
.60
.80
.45
.27
.85
3.1
3.5
.18
1.2
3.1
.82
.58
.31
.80
.95
.18
.82
3.2
3.1
.18
.34
1.1
1.2
.39
1.6
1.2
.70
.92
.68
.80
.40
.79
.71
.95
.60
.14
.48
1.3
1.0
.08
.77
1.2
.65
.36
.39
1.7
2.4
.18
.82
1.4
1.6
.15
2.9
1.8
4.1
.55
2.9
2.6
4.2
.32
1.7
1.7
.75
.32
2.2
1.9
.20
1.1
1.2
4.8
2.8
.34
1.4
2.4
1.4
.36
1.1
2.0
3.9
.59
1.5
3.1
3.0
.59
1.8
1.2
.80
.16
1.2
1.4
1.2
.60
1.7
.20
.35
.11
.70
Ti0
2
0.32 .29
.24
.09
.20
.15
.14
.14
.26
.25
.14
.42
.17
.12
.17
.24
.19
.16
.20
.21
.79
.32
.16
.52
.52
.36
.44
.18
.15
.08
P20
5
0.24 .26
.27
.24
.25
.24
.25
.24
.06
.24
.25
.35
.24
.22
.23
.24
.24
.29
.23
.26
1.2 .41
.21
.31
.25
.51
.36
.25
.22
.25
mo
0.07 .07
.31
.31
.05
.08
.05
.05
.05
.05
.09
.06
.08
.04
.07
.09
.06
.06
.06
.12
.12
.11
.08
.16
.12
.13
.12
.05
.04
.09
00?
<.05
<.05
<.05 .08
.05
2.5
<.05
<.05
<.05
<.05
<.05
<.05
<.05 .05
.05
.05
.05
.05
.05
.11
.65
.05
.05
.05
.05
.05
.18
.11
.05
.12
Sum
95 93 92 91 92 97 94 98 78 98 97 93 97 94 90 94 90 94 88 96 100
95 96 99 91 96 96 93 97 84
Table 20. Summanj log of drill hole WS-9
Interval Description (meters)_____ _____
0-35 Diorite, fine-grained (little core15-35 m)
35-42 Diorite, fine- to coarse-grained,slightly pyritic
42-45 Pyrrhotite, 90 percent sulfide45-46 Andesite with pyrite and pyrrhotite,
5-10 percent sulfide46-50 Pyrrhotite, some pyrite, 40-60
percent sulfide
50-51 Diorite, some pyrrhotite, <5 percentsulfide
51-53 Pyrrhotite, some pyrite, 60-80percent sulfide in diorite. Faults at 53 m at acute angle to axis of core
53-67 Diorite, trace pyrrhotite67-76 Brecciated zones cemented by
pyrrhotite, pyrite, and calcite in andesitic sedimentary rock, calc-silicate rock, and chloritic and kaolinitic diorite
76-89 Diorite; chloritic and calc-silicaterock, slightly pyritic
89-91 Calc-silicate rock, brecciated ,pyritic
91-93 Diorite, chloritic93-106 Argillite, calc-silicate, contorted 106-111 Diorite, brecciated in part, calcite
veins111-117 Argillite and calc-silicate; breccia
zone with calcite veining and cement. Structures about parallel to axis of core
117-129 Diorite, chloritic, and argi31ite.Brecciated 122-123 m with some pyrrhotite and pyrite
129-142 Pyrrhotite, massive, 80-90 percentsulfide
142-143 Diabase143-154.4 Argillaceous calc-silicate rock,
contorted
45
Table 21. Analyses of core from drill hole WS-9
[nil = not detected. Copper results in parts per million, silver and gold in ounces per ton. Material analyzed: MP, massive pyrite; DP, disseminated pyrite. Fire assays for gold and silver by S.M. Bahijri, chemical analyses for copper by Ibrahim Baradja, spectrographic analyses by K. Shahwan, USGS-DGMR Chemical Laboratory]
CopperSample number
3500335005350063500735008
3501135013350193502035024
35027350293503135033
Interval (meters)
374242.54343.5
4446
120123129
130137138141
Spectro graphic
3010101020
15010151520
20201515
Chemical
3010101010
1010101010
10<10<10<10
GoldFire
nilnilnilnilnil
nilnilnilnilnil
nilnilnilnil
Silverassay
nil0.10.17.17.13
.11
.14
.16
.28
.16
.06
.17
.05
.11
Material analyzed
DPDPMPMPMP
MPMPDPDPMP
MPMPMPMP
46
Table 22. Major
elem
ent
chemical an
alys
es of
core from d
rill
ho
le W
S-9
[* in
dica
tes
tota
l S
and
Fe,
respectively.
Rapi
d ro
ck ana
lyse
s un
der
the
dire
ctio
n of L.
Shapiro, US
GS La
bora
tory
, Washington,
D.C.]
Sample
number
35003
3500
535006
3500
735
008
3501
135
013
35019
35020
35024
3502
735029
3503
13503
3
Interval
(met
ers)
37 42 42.5
43 43.5
44 46 120
123
129
130
137
138
141
SiOz
48.1
15.4
10.8
19.8
43.2
23.2
16.7
39.4
42.4 9.1
7.8
6.7
9.0
10.3
A120
3
8.0
5.6
3.8
5.4
9.0
5.7
4.3
11.4
12.2 2.3
2.4
2.2
3.2
3.4
S* 2.6
26.0
21.0
20.9 4.6
19.9
32.4 5.4
1.2
20.5
22.6
25.8
27.0
30.9
Fe*
6.8
39.9
50.6
42.5
15.9
35.4
35.0 7.8
5.8
52.2
53.2
53.2
48.2
43.4
MgO
15.2 2.1 .86
.84
8.1
2.2
1.8
5.2
5.5 .91
.56
.52
.85
.53
CaO
Na20
K20
(Res
ults
in weight
11.4 1.8
1.1 .70
.94
2.5
1.2
8.8
8.6
1.9 .95
1.0
1.0
.85
0.94 .62
.71
1.2
1.5 .90
.57
1.8
1.8 .38
0 .02
.29
.23
0.65 .37
.37
1.5 .45
.72
.52
.80
1.4 .45
.32
.08
.62
.22
H20-
H2O
percent)
0.18 .90
.21
.10
.25
.52
.66
2.7 .39
.30
.35
.57
.78
1.6
2.4
2.3 .56
.84
2.0
2.8
3.2
6.1
8.3 .90
.65
.63
1.0
1.7
Ti02
0.44 .30
.15
.31
.36
.26
.25
1.0 .79
.11
.11
.06
.12
.14
PzQs
0.40 .30
.26
.26
.59
.24
.19
.34
.44
.21
.23
.23
.23
.22
MnO
0.18 .12
.04
.05
.29
.14
.07
.09
.14
.12
.08
.05
.14
.07
<X>2
0.08
<.05
<.05
<.05 .21
1.6
3.0
8.8
10.2 .5
2
.05
.05
.05
.05
Sum 97 96 90 94 87 96 100
100 99 90 89 92 92 94
Area J gossan
The area J gossan covers an area of 10,390 sq m and is a discontinuous zone about 500 m long and 10 to 40 m wide. The zone is truncated by granitic bodies to the north and south and by a dioritic body to the east.
Analyses of surface samples are given in appendix 1.
Area K gossan
The area K gossan is 400 m long and is 15 to 60 m wide; it covers an area of 14,790 sq m. It ends against granitic rocks to the north and dioritic rocks to the east and is overlapped by alluvium in a tributary of Wadi Mahal on the south .
Analyses of surface samples are given in appendix 1.
Area L
Area L covers an area of 60,760 sq m and is shown in the southwestern part of the plate. The principal gossan zone has an overall length of about 750 m and a width of as much as 200 m. The area contains discontinuous gossan bodies that are separated by septae of granite and diorite intrusive bodies and probably underlain by intrusive rocks at shallow depths.
Samples along several lines cut across the area. The analyses of these samples are given in appendix 1.
Geochemistry
Minor elements in pyrite-pyrrhotite-bearing core from Wadi Wassat are present in comparatively low abundances. Precious metals are virtually absent, base metal abundances are low, and many other elements are present in amounts below their detection limits (Overstreet and others, 1976).
In drill holes WS-6 and WS-7, Overstreet and others (1976) found that 16 elements, antimony, arsenic, beryllium, bismuth, cadmium, germanium, gold, silver, tin, lanthanum, niobium, selenium, tellurium, thallium, tungsten, and vanad ium, are present in both the massive sulfide-bearing material and the wall-rock material in amounts below the limits of analytical detection for the methods used. Minor elements present in greater amounts in the massive sulfide-bearing material than in the wall-rock material are boron, cobalt, gallium, lead, molybdenum, and tin. The minor elements that are more abundant in the wall-rock material than in the sulfide-bearing material are barium, chromium, copper, lith-
48
ium, manganese, mercury, nickel, rubidium, scandium, titan ium, vanadium, yttrium, zinc, and zirconium.
Results of analytical work
Approximately 1100 samples from Wadi Wassat were analyzed in the USGS-DGMR Chemical Laboratory in Jiddah. Of these, about 450 were gossan samples and 650 were sulfide-bearing samples from drill core. In addition to nickel and cobalt, silver, copper, lead, zinc, manganese, chromium, and molyb denum were routinely determined; gold was also determined in some samples. These analytical determinations were entered in the DGMR PDP-11/45 computer, and the means and correlation coefficients were calculated.
Resources
Mapping in the Wadi Wassat area indicates that about 765,000 sq m of gossans are exposed (plate). Some of these gossans were explored and found to grade into sulfide-bearing units at a depth of about 30 m. The calculation of sulfide resources is subject to some uncertainties, but using reason able assumptions, estimates of the minimum available tonnage can be made.
During exploration, the percentage of pyrite and pyrr- hotite in each unit of core was estimated, and the unit was placed into one of the following classes: 100-80 percent sulfide, 80-50 percent sulfide, and 50-10 percent sulfide (table 23). The total length of each class was then divided by the total aggregate length, giving the following percentages of each class:
100-80 percent - 53 percent of total mineralized interval 80-50 percent - 6 percent of total mineralized interval 50-10 percent - 41 percent of total mineralized interval
Hole WS-5 was excluded from the computation, because it ex plored a stratigraphically higher bed that is not considered to be representative of the other mineralized beds.
The computation of tonnage of sulfide ore was carried out as follows:
The percentage of sulfide-bearing material containing more than 80 percent sulfide (53 percent) is multiplied by the specific gravity of pyrite (5.0), and then by the total square meters (less areas J, K, and L, 678,520 sq m) of gos san (appendix 1) to give metric tons per meter depth. Thus .53 x 5.0 x .80 x 678,520 x 100 = 143,846,240 (total metric tons per 100 m depth) .
49
Table 23. Distribution of pi/rite and pyrrhotite in drill holes WS-1 through WS-9
[Thickness computed on assumption that all bedding is vertical]
Hole number
1
3
4
5
6
7
8
9
Cumulative length (meters) Percent sulfide class
100-80 80-50 50-10
25
52
52
7
26
52
41
16
6
10
2
2-
-
5
2
37
18
23
70
14
28
15
4
Total
68
80
77
79
40
80
61
22
50
On the assumption that the interval from the surface to the bottom of the oxidized zone (averaging about 25 m) to the bottom of the holes (averaging about 100 m) is 80 percent sulf ide-bearing ore, then the resources are 75 percent of 143,846,240, or 107,884,680 tons, which can be rounded off to 107,500,000 tons. This iron sulfide resource averages about 40 percent iron and 35 percent sulfur.
In addition, large blocks in areas J, K, and L, which may be underlain by sulfide-bearing material, were not included in the calculations, and therefore the resources calculated above represent a minimum value. In order to obtain a more accurate idea of the total available tonnage, additional drilling both along strike and down dip is required.
51
REFERENCES CITED>
Akhrass, M. N. , 1966, Magnetic survey on the gossan of Wadi Wassat (near Bi'r Idimah): Saudi Arabian Directorate General of Mineral Resources Open-File Report 267, 2 p.
Alien, R. V., and Davis, W. E., 1969a, Geophysical investigations in theBi'r Idimah-Wadi Wassat area, Saudi Arabia Part One: U.S. Geological Survey Open-File Report (IR)SA-53, 3 p.
_________ 1969b, Geophysical investigations in the Bi'r Idimah-Wadi Wassat area, Saudi Arabia Part Two: U.S. Geological Survey Open-File Report (IR)SA-54, 4 p.
Anderson, R. N. , and Halunen, A. J., 1974, Implications of heat flow for metallogenesis in the Bauer Deep: Nature, v. 251, p. 473-75.
Brown, D. G. , and Jackson, R. 0., 1959, Geology of the Asir quadrangle, Kingdom of Saudi Arabia: U.S. Geological Survey Miscellaneous Geologic Investigations Map I-217A, scale 1:500,000.
Cohee, G. C. , 1974, Stratigraphic nomenclature in reports of the U.S. Geological Survey: Washington, D.C., Geologic Names Committee, 45 p.
Corliss, J. G., 1971, The origin of metal-bearing submarine hydrothermal solutions: Journal of Geophysical Research, v. 76, p. 8128-8138.
Dodge, F. C. W., and Rossman, D. L. , 1975, Mineralization in the Wadi Qatan area, Kingdom of Saudi Arabia: U.S. Geological Survey Saudi Arabian Project Report 190, 71 p. (U.S. Geological Survey Open-File Report 75-309).
Goodwin, A. M., 1973, Archean iron-formations and tectonic basins of the Canadian Shield: Economic Geology, v. 68, p. 915-933.
Greenwood, W. R., 1980, Reconnaissance geology of the Wadi Wassat quadrangle sheet 18/44 C, Kingdom of Saudi Arabia: Saudi Arabian Directorate General of Mineral Resources Geologic Map GM-40, 52 p., scale 1:100,000.
52
jacKaman , Barry, 1972, Genetic and environmental factors controlling the formation of the massive sulfide deposits of Wadi Bidah and W'adi Wassat, Saudi Arabia: Saudi Arabian Directorate General of Mineral Resources Technical Record, TR-1972-1, 244 p.
Kuno, H., 1966, Lateral variation of basalt magma type across continental margins and island arcs: Bulletin Volcanologique, v. 29, p. 195-221.
Martin, Conrad, 1973, Wadi Wassat pyrite, in Mineral resources research, 1968-69: Saudi Arabian Directorate General of Mineral Resources, p. 94-96.
Mauger, R. L. , 1972, A sulfur isotope study of the Ducktown Tennessee district, U.S.A.: Economic Geology, v. 67, p. 497-510.
McMurty, G. M., and Burnett, W. C. , 1975, Hydrothermal metallogenesis in the Bauer Deep of the southeastern Pacific: Nature, v. 254, p. 42-44.
Overstreet, W. C. , 1968a, Mineral investigations between Khamis Mushayt and Bi'r Idimah, Saudi Arabia: U.S. Geological Survey Open-File Report (IR)SA-23, 18 p.
_________ 1968b, Mineral exploration between Bi'r Idimah and Wadi Haraman, Asir quadrangle, Saudi Arabia: U.S. Geological Survey Open-File Report (IR)SA-39, 70 p.
________ 1968c, Preliminary results of a trip October 30-December 21, 1965, to the area between Sha'ya and Jabal Bani Bisqan, Saudi Arabia, together with a synopsis of mineral reconnaissance in the Asir quadrangle: U.S. Geological Survey Open-File Report (IR)SA-40, 48 p.
________ 1969d, Summary of results from a trip February 6-March 5, 1966, to Bi'r Idimah, Jabal Ashirah, and the As Sarat mountains, Saudi Arabia: U.S. Geological Survey Open-File Report (IR)SA-49, 47 p.
Overstreet, W. C., Bahijri, S. M., Fourati, M. A., and Gonzales, Louis, 1967a, Progress Report II. Assays and analysis of pyritic core from Wadi Wassat gossan, Saudi Arabia: U.S. Geological Survey Open-File Report (IR)SA-63, 8 p.
Overstreet, W. C., Bahijri, S. M., and Shararahly, A. H., 1969a, Results of a trip October 25-29, 1966, to the Bi'r el Adhbat area and the Esh Qay'ib (Esh Sha'ib) mine, eastern Asir, Saudi Arabia, including assays of materials from ancient mines in the eastern Asir: U.S. Geological Survey Open-File Report (!R)SA-84, 20 p.
Overstreet, W. C., Gonzalez, Louis, Thompson, C. E., Fourati, M. A., Sharah, All, and Sumbul, Jamal, 1967b, Progress report on analyses of pyritic core from diamond drill holes under gossan at Wadi Wassat, Saudi Arabia: U.S. Geological Survey Open-File Report (IR)SA-58, 17 p.
Overstreet, W. C., Hubert, A. E. , Crenshaw, G. L. , , and Mosier, E. L., 1976, Petrogenic significance of minor elements in pyritic core from the Wadi Wassat massive sulfide deposit, Kingdom of Saudi Arabia: U.S. Geological Survey Saudi Arabia Project Report 214, 116 p. (U.S. Geological Survey Open-File Report 76-863).
Overstreet, W. C., Raisanen, Eino, Fourati, M. A., Shahwan, K. H., and Baradja, Ibrahim, 1969b, Progress Report III. Description and analyses of pyritic core from drill holes 6 and 7, Wadi Wassat area: U.S. Geological Survey Open-File Report (IR)SA-92, 75 p.
Overstreet, W. C., and Rossman, D. L., 1970, Reconnaissances geology of theWadi Wassat quadrangle, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report (IR)SA-117, 67 p.
Roberts, Ralph, J., 1976, The genesis of disseminated and massive sulfide deposits in Saudi Arabia: U.S. Geological Survey Saudi Arabian Project Report 207, 54 p. (U.S. Geologicval Survey Open-File Report 76-602).
Rye, R. 0., Roberts, R. J., and Mawad, M. M. , 1979, Preliminary sulfur isotope investigations of mineral deposits in the Precambrian Shield, Kingdom of Saudi Arabia, in Evolution and mineralization of the Arabian-Nubian Shield: Oxford, Pergamon Press, v. 1, p. 131-140.
Weissenborn, A. E., and Earhart, R. L., 1969, Appraisal of the Wadi Wassat and Wadi Adhbat pyrite deposits, Asir quadrangle, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report (IR)SA-lOl, 21 p.
Wilch, L. 0., 1978, Rock analysis storage system (RASS), Saudi Arabia - An introduction to the system and sample submittal manual - 1978, with a. section on Keypunching . instructions by L. 0. Wilch, and L. D. North: U.S. Geological Survey Saudi Arabian Project Report 241, 42 p. (U.S. Geological Survey Open-File Report 79-591).
Wright, C. M., 1965, Syngenetic pyrite associated with a Precambrian iron ore deposit: Economic Geology, v. 60, p. 998-1019.
54
A.
APPENDIX 1
List of surface sample areas (gossans) and sample numbers
Area A
87892-897 87938-939
Area B
87850-863 87864-873 87874-881 87882-889 87890-891
Area C
87824-829 87830-835 87836-838 87839-849
Area D
87811-815 87816-823
Area E
87730-749 87750-774 87775-810 87898-914
Area F
87718-729
Area G
87681-717
Area H
87645-655 87656-680 87915-922
Area I
87586-600 87601-611 87612-622 87623-624 87625-629 87630-639 87640-644 87923-939
Area J
87569-585
Area K
87553-568
Area L
87470-477 87500-506 87507-531 87532-533 87534-545 87546-552
55
B* Areas of gossan blocks (in square meters)
A. 17,519
B. 105,114
C. 19,876
D. 24,239
E. 289,778
F. 34,912
G. 35,620
H. 74,582
I. 76,897
J.
K.
L.
SUBTOTAL
10,930
14,788
60,759
TOTAL
17,520
105,110
19,880
24,240
289,780
34,910
35,600
74,580
76,900
678,520
10,930
14,790
60,760
765,000
not included
in tonnage cal
culations
56
C. Descriptions and geochemical data for gossan samples
Description codes (pages 58-66); Wilch, 1978)
Column* Field Code Meaning
11 rock type A12 sample type B13 sample source A14 rock type Y17 matrix A19 oxidation state A21 ore minerals D22 mineral deposit
form D 24 geologic age D
25-26 rock name GO 28 area
29 subarea
rockcompositeoutcropothersilicaoxidizedother
massive sulfidelate Precambriangossanalphabetic code refersto areas as on figure2 (see text, p. 21)numeric code (seeBlain, 1981, fig. 13,for location ofsubarea)
* numbers read vertically on listing
Geochemical data: AA, atomic absorption analysis; P, partial digestion; T, total digestion; CM, colorimetric analysis. Cu, copper; Pb, lead; Zn, zinc; Ag, silver; Co, cobalt; Ni, nickel; Mo, molybdenum; Cr, chromium; Mn, manganese. N, not detected at value stated; L, less than value stated; B, not analyzed.
57
RASS II - ROCK ANALYSIS STORAGE SYSTEM FOR GEOCHEMICAL DATA PROGRAM NO* B860 ( 3/ 1/79)
SAMPLE LAST DATE PROJECT MISSION FIELD NO ID UPDATE SUBMITTED NO
874708747187472874738747487475874768747787501875028750387504875058750687507875088750987510875118751287513875148751587516875178751887519875208752187522875238752487525875268752787528875298753087531875328753387534875358753687537875388753987540875418754287543
8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-8-
1-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-101-10
MO1-101-101-101-101-10
78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-78-
1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-
111111111111111111111111111111111111111111111111111
516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516516
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JOB NO
HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554HM554
11111111234567
A B A YA B A YA B A Y AA B A Y AA B A Y AA B A Y AA B A Y AA B A Y AA B A Y AA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A Y AA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A Y
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CODED2222234567
D G 0D 6 0D G 0D G 0D G 0D G 0D G 0D G 0D 6 0D G 0D G 0D G 0D G 0D G 0D G 0DG 0DG 0D G 0D G 0D 1 0D 6 0D G 0D G 0D G 0D G 0D 6 0D G 0060D 6 0D G 0D 6 0D G 0D G 0D G 0D G 0D G 0D G 0D G 0D G 0D G 0D G 0D G 0D G 0D G 0D G 0D 6 0D G 0D 6 0D G 0D 6 0D G 0
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L 1L 1L 1L 1L 1L 1L 1L 1L 1L 1L 1L 1L 1L 1L 2L 2L 2L 2L 2L 2L 2L 2L 2L 2L 2L 2L 2L 2L 2L 2L 2I 2L 2I 2L 2L 2L 2L 2L 2L 3L 3L 3L 3L 3L 3L 3L -5L 3L 3L 3L 3
58
RASS II - ROCK ANALYSIS STORAGE SYSTEH FOR GEOCHEHICAL DATA PROGRAH MO, B860 ( 3/ 1/79)
SAMPLE LAST BATE PROJECT MISSION FIELD NO ID UPDATE SUBMITTED NO
JOB NO CODED DATA 3 3 0 5
8754487545875468754787548875498755087551875528755387554875553755687557S7558875598756087561Q-JC inG/ iJUi
3756387564me/r u/ ijOo
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A B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A Y AA B A Y AA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YA B A YBAYBAYBAYB A V
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59
RASS II ROCK ANALYSIS STORAGE SYSTEM FOR GEOCHEHICAL DATA PROGRAM NO, B36C ( 3/ 1/79)
3AHPLE LAST BATE PROJECT MISSION FIELD ID UPDATE SUBMITTED NO
JOB NO C 0 D E B
8 -ICIjC 1 \>1 *J
8 -ICQl i J7O
S-icn-i / -SI i
3759887599876003760107602876033760487605376063760787608376098761037611876123761307614376158761637617876183761987620 "p<n <\Jl Oi.1
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SAMPLEIB
3764?876483764937650376518T/CT /Out
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376548765537656o/ 6j/876583765?3766C8766187662376633766437665376663766737663376693767087671876723767337674d/ O/ a
8767637677876733767987680376C137682C76833768437685376863768737688376893769087691876928769337694076953769737698
LASTUPBATE
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FIELB NO JOB NO
HH554MH554IJUCC*nnuvrt
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RASS II - ROCK ANALYSIS STORAGE SYSTEH FOR GEOCHEHICAL DATA PROGRAH NO, B860 ( 3/ 1/79)
SAHPLE LAST DATE PROJECT HISSICN FIELD NO ID UPDATE SUBMITTED NO
37699377003770137702377038770437705377063770787708377098771037711877123771337714377153?7163 -i-n -r 'in
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62
RASS II - ROCK ANALYSIS STORAGE SYSTEM FOR GEOCHEHICAL DATA PftOGRAH NO, B860 ( 3/ 1/79)
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SAW.E LATITUDE LOMSITUD AA-HN-P
8753587536875378753887539
8754087541875428754387544
8754587546875478754887549
8755087551875528755387554
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8756587566875678756887569
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60*000050.000035*0000
250.0000180.0000
170.000035.000055.000070.0000115.0000
270.000035.000055.000070.000095,0000
110.0000160.0000250.000075.000070.0000
35.000045.000040.0000215.0000215.0000
170,000025.000035.000090.000030.0000
95.000090.0000160,0000220.0000230.0000
160.0000210.0000120.0000115.0000140.0000
85.000085.0000
70
GOSSANS AT WADI UASSAT KINGDOM OF SAUDI ARABIA (CONTINUED)
SAMPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-CO-P AA-NI-P AA-AG-T Crt-MO CM-CR
B757787578875798758087581
8758287583875848758587586
87587B7588875898759087591
8759287593875948759587596
875978759887599S760087601
8760287603876048760587606
8760787608876098761087611
8761297613376143761597616
8761787618
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200,0000300,0000500,000085,000050,0000
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85,0000600,000090,000070,000065,0000
500,000060,0000
71
GOSSANS AT UADI UASSAT KINGDOM OF SAUDI ARABIA (CONTINUE*)
SAMPLE LATITUDE LONGITUD AA-MN-P
8757787578875798758087581
8758287583875848758587586
8758787588875898759087591
8759287593875948759587596
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170.0000165.0000155.0000190.0000220.0000
95.0000115.0000110.0000140.0000165.0000
165.0000160.0000200.0000185.0000120.0000
120.0000185.0000
72
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SAMPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-CQ-P AA-NI-P AA-AG-T CM-MO CM-CR
3761987620876218762287623
8762587626876278762887629
3763087631876328763387634
8763587636876378763887639
3764087641876428764387644
376458764687647S764887649
8765037651876528765387654
8765587656876578765887659
8766087661
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GOSSANS AT WADI UASSAT KINGDOM OF SAUDI ARABIA (CONTINUED)
SAMPLE LATITUDE LON6ITUD AA-MN-P
8770587706877078770887709
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GOSSANS AT UADI HASSAT KINGDOM OF SAUDI ARABIA (CONTINUED)
SAMPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-CO-P AA-NI-P AA-AG-T CM-HO CM-CR
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GOSSANS AT WABI WASSAT KINGDOM OF SAUDI ARABIA (CONTINUED)
SAMPLE LATITUDE LONGITUD AA-MN-P
8774737748877498775087751
8775287753877548775587756
8775787758877598776087761
877628776387764S776587766
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GOSSANS AT KADI UASSAT KINGDOM CF SAUDI ARABIA (CONTINUED)
SAHPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-CO-P AA-NI-P AA-A8-T Ch-hQ CH-Cft
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GOSSANS AT yADI WASSAT KINGDOM OF SAUDI ARABIA (CONTINUED)
SAMPLE LATITUDE LON6ITUD AA-MN-P
8778987790877918779287793
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GOSSANS AT WADI WASSAT KINGDOM OF SAUDI ARABIA (CONTINUED)
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400,0000225,0000110,0000140,0000700,0000
140,0000150,0000115,0000600,0000225,0000
190,0000210,0000700,000090,000040,0000
115,0000675,0000125,0000120,0000115,0000
250,0000240,000070,000080,0000300,0000
90,000040,000035,0000175,000035,0000
30,000040,0000
83
GOSSANS AT WADI JJASSAT KINGOON OF SAUDI ARABIA (CONTINUED)
SAHPLE LATITUDE LONGITUD AA-MN-P
8783287833878348783587836
8783787838878398784087841
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1313221313
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28E28E47E29E30E
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84
GOSSANS AT WABI UASSAT KINGDOM OF SAUDI ARABIA (CONTINUED)
SAMPLE LATITUDE LON6ITUD AA-CU-P AA-PB-P AA-ZN-P AA-CO-P AA-NI-P AA-AG-T CH-HO CH-CR
8787487875878768787787878
8787987880878818788287883
8788487885878868788787888
8788987890878918789287893
8789487895878968789787898
8789987900879018790287903
8790487905879068790787908
8790987910879118791287913
8791487915
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2218 2318 2418 24
18 2418 2418 2418 2418 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
IS 2118 20
31N31N31N31N31N
31N31N31N27N27N
27N27N27N27N27N
27N42N45N05N05N
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44 13 30E44 13 39E44 13 29E44 13 17E44 13 17E
44 13 17E44 13 18E44 13 19E44 13 19E44 12 42E
44 12 42E44 12 43E44 12 44E44 12 44E44 12 45E
44 12 46E44 12 46E44 12 47E44 12 48E44 12 49E
44 12 49E44 12 Jk)E44 12 51E4', 12 52E44 12 52E
44 12 53E44 12 22E
30.000015.000015.000015.000015.0000
10.000015.000025,000025.000025.0000
30.000025.00005.000010.000010.0000
10.00005.000030.000010.000010,0000
10,00005,000020,000030,000015,0000
10,000010,000010,000010,000010,0000
5,000010,000030,000050,000040,0000
10,000020,00005,000010,000010,0000
15,000020,0000
20,000030,000015,000020,000030,0000
10,000010,000015,000045,000015,0000
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20,000020,000025,000020,000020,0000
35,000015,000020,000015,000020,0000
10.0000L10,000010,000025,000010,0000
15,000010.0000L35,000015.000010,0000
20,000020,000015,000015,000010,0000
30,000020,0000
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10,000015,000020,000025,000020,0000
15,000020,000020,000010,000020,0000
15,000025,000015,000030,000015,0000
20,000010,000020,000025,000020,0000
10,000010,000010,000020,000010,0000
10,000010,000040,000030,000025,0000
20,000020,000015,000020,000015,0000
20,000020,0000
25,000010,000010,000020,000020,0000
15,000015,000015,000030,000020,0000
10.0000L10,000010,000010.0000L15,0000
15,000010,000030,000015,000025,0000
25,000025,000015,000020,000015,0000
10.0000L10,000010,OOOOL15,000010,OOOOL
10,000010,OOOON35,000040,000020,0000
25,000015,000015,000010,000010.0000
25,000030,0000
20,000040,000030,000035,000025,0000
30,000035,000020,000025,000030,0000
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30,000030,000045,000035,000050,0000
20,000020,000030,000035,000020,0000
30,000030,000035,000020,000035,0000
20,000020,000025,000040,000030,0000
45,000025,000035,000030,000015,0000
25,000030,0000
0,5000N2,50001,75002,50000.5000N
1,75002,50003,00000.5000N1,7000
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60,000030,0000
700,000035,000040,000060,0000325,0000
90,0000100,0000200,0000225,000050,0000
60,000080,0000750,000030,000030,0000
35,0000275,000040,000060,000030,0000
1200,000035,000085,000050,0000300,0000
40,0000195,000070,0000150,0000105,0000
120,0000155,00001000,000090,000080,0000
70,0000150,000070,000050,000070,0000
150.000060,0000
85
GOSSANS AT UADI UASSAT KINGDOM OF SAUDI ARABIA (CONTINUED}
SAHPLE LATITUDE LONGITUD AA-HN-P
8787487875878768787787878
8787987880878818788287883
8788487885878868788787888
8788987890878918789287893
8789487895878968789787898
87399&7900879018790287903
8790487905879068790737908
8790987910879118791287913
8791487915
1818181818
1818181818
1818181818
1818181818
1313181818
1818181318
18181818IB
1818181818
1818
2323232323
2323232323
2323232323
2322232424
2424242421
2121212121
2121212121
2121212121
2120
31N31N31N31N31N
31N31N31N27N27N
27N27N27N27N27N
27N42N45N05N05N
05N04N04N04NUN
IONIONIONIONION
ION09N09N09N09N
09NmOSN08NOSN
08N14N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1313131313
1313131313
1313131313
1313131313
1313131312
1212121212
1212121212
1212121212
1212
27E28E28E29E29E
30E30E31E27E27E
28E28£29E29E30E
30£39£29E17E17E
17E18E19E19E42E
42E43E44E44E45E
46E46E47E48E49E
49E50E51E52E52E
53E22E
95, 000075,000085,
125,00000000
125,0000
85,85,
110,175,145,
170,
00000000000000000000
0000225,000080,000055,75,
65,115,55,100,30,
45,30,40,
350,45,
125,70,75,
00000000
00000000000000000000
00000000000000000000
000000000000
215,0000125,
100,160,65,
400,115,
65,55,75,65,90,
155,
0000
00000000000000000000
00000000000000000000
0000175,0000
86
2,8
0000 '0210000 'S2V0000 '0010000 '58
0000*0210000 '00010000 '0120000 'S20000 '06
0000 *OS£0000 *OVOOOO'SOI0000 '080000 'S28
0000*060000 '080000 '0V0000 '0060000 'SV
0000 'OS0000 'SV0000 '002OQOQ'OV0000 'OS
0000*02OOOO'Sl0000 'SOOOO'OI
0000 '010000 'SOOOO'OI0000*01OOOO'Sl
0000'02OOOO'OI0000 'S0000 'SOOOO'OI
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OOOO'OIOOOO'SlOOOO'Sl0000 *S!0000 '0£
0002*1NOOOS'OOOOS'20002*1
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0000*S20000*S20000 '0V0000 *0£
0000 *0£0000 '090000 '0£0000 '0V0000' SV
0000 *S20000 *OV0000 'S£0000 '0V0000 'S2
0000 '0£0000 *OV0000*020000*090000 *SV
0000 '0£0000* S£0000 *S20000 *S20000*S3
10000*010000 *0£0000 *0£0000 *S2
0000*510000 *0£0000*520000 '020000 'S2
0000*020000*020000* 0£0000 '020000 '02
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0000*020000*0£0000*S20000*020000 '02
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0000'S20000 *0£0000 *S£0000 *S£0000*02
0000*020000 '020000 'SS0000 '020000 *S2
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0000 'S20000*090000 'SV0000*090000 'S£
0000 '0£0000 'S20000 '0£OOOO'SlOOOO'Sl
381 £1 VV391 £1 VV32V II VV32V II VV
32V II VV32V II VV32V II VV39V II VV39V II VV
39V II VV3SV II VV3SV II VV3SV II VV3VV II VV
3VV II VV3VV II VV3VV II VV3V2 21 VV3V2 21 VV
3V2 21 VV3£2 21 VV3£2 21 VV3£2 21 VV322 21 VV
N02 V2 81N02 V2 81N9S 02 81N9S 02 81
N9S 02 81N2S 02 81N2S 02 81N2S 02 81N8S 02 81
N8S 02 81N8S 02 81N8S 02 81N8S 02 81N8S 02 81
N8S 02 81N8S 02 81N8S 02 81N9I 02 81N9I 02 81
N9I 02 81NSI 02 81NSI 02 81NSI 02 81NVI 02 81
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S£628V£628££6282£628r jttOtlO
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GOSSANS AT UADI fcASSAT KINGDOM OF SAUDI A8ABJ
SAHPLE LATITUDE LON6ITUD AA-MN-P
8791637917379188791987920
87921879228792387924S7925
8792687927879288792987930
8793187932879338793487935
8793687937S793887939
1818181818
1818181818
1818181818
1818181818
18181818
2020202020
2020202020
2020202020
2020202020
20202424
14N15N15N15N16N
16N16H58N58N58N
58H58K5SN58H58N
58N57N57N57N56*
56N56N20N20N
4444444444
4444444444
4444444444
4444444444
44444444
1212121212
1212111111
1111111111
1111111111
11111313
22E23E23E23E24E
24E24C44E44E44E
44E45E45E45E46E
46E46E47E47E47E
47E47E16E18E
50 ,000045,00009570120
15024012012565
80851205550
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45,70909540
145150
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00000000
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000000000000oooc0000
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00000000
55,000080 , 0000
D0039 - STOP
88
APPENDIX 2
A.
Locations, altitudes, azimuths, and inclinations of
diamond drill holes
[Elevations by Wallace an
d Tiernan Altimeter calibrated in 10
-m divisions, referred to
reference points an
d existing 1:10,000-scale 10
-m contour interval topographic map. Holes
located on
1:14,000-scale pl
ates
. Geodetic locations referred to Station "A
stro
" as
located on
1:50,000-scale photomosaic sheet 9F
, covering lat
18°15' to 18°30' N. ;
lo
ng
44°00' to
44°30' E.
Location of "Astro", lat
18°24'41" N.
, long
44°13'13" E.
]
Dril
l number
WS-1
CD
WS-2
oWS-3
WS-4
WS-5
WS-6
WS-7
WS-8
WS-9
Approximate location
latitude
(nor
th)
18°2
4'06
"
18°2
3'16
"
18°2
3I13"
18°2
3'45
"
18°24'04"
18°20'35"
18°21'20"
18°20'21"
18°21 '16
"
longitude
(eas
t)
44°13'16"
44°13'32"
44°13'34"
44°13
I27"
44°13'20"
44°12'43"
44°13'03"
44°12'18"
44°11'35"
Approximate
elevation
(meters)
1,203
1,21
4
1,215
1,200
1,201
1,235
1,225
1,244
1,265
Direction
S.67
°E.
West
West
N.80
°E.
S.72
°E.
S.67
°E.
N.65°W.
N.45°E.
N.75°W.
Inclination
-45°
-45°
-45°
-45°
-60°
-45°
-45°
-45°
-45°
Depth
(met
ers)
139.5
37.0
158.6
129.9
103.0
91.5
138.5
152.6
154.4
Remarks
Aborted
Pyrrhotite
Pyrrhotite
1,100.0
B. List of samples from drill holes
[Zones are indicated on drill holes section, figure 6. Lithology: V-S, volcanic and sedimentary rocks; D sul, disseminated sulfides; M sul, massive sulfides; D + M sul, disseminated and massive sulfides. Areas shown on figure 2]
Depth (meters) Sample numbers Zones Lithology
Area A
WS-1
0-30
30-51
48.75-58
58-75
75-80 80-83 83-101.4
101.4-113
113-132.6
WS-5
0-50
54-56.5 54-70.1
70.1-78 73-89.4
90-103
Area C
WS-3
0-29.5 29.5-37 37-47
47-59 59-79 62-67
79.3-94
107010-107012
107013-017025 107282-107286 107214-107221
107222-107238
107239-107241 107242-107244 107027-107052 107245-107256
107257-107,281
107413-107446
107159-107160 107447-107461 107462-107470 107161-107169
107471-107482
107287-107302 107303-107309 107310-107314
107057-107064 107065-107084 107315-107318 107085-107098
1 0-30 m
30-^3 2
43-58
3 58-75
75-86 4 86-109
109-113
5 113-139
1 0-50
2 50-73 73-83 83-90
3 90-103
1 0-47
2 47-94
Gossan + V-S
M sul
D sul
V-S
D sul Msul D sul
V-S
D sul
D + M sul M sul D sul
V-S
V-S
M sul
91
B. List of samples
Depth (meters)
WS-3 (cont.)
94-9696-101 103-121 101-121 121-132
133-153.6
Area B
WS-4
0-28
28-^3 28-43 43-56.4 55-64.9
64.4-74
74-85.3 85-95.5 92-94.5
95.5-117
117-129.9
Area F
WS-6
0-35 35-63 63-91.5
Area E
WS-7
0-24
24-8467-67.582-82.5
84-126
126-138.5
from drill holes
Sample numbers
107099-107100 107319-107323 107101-107116 107324-107327 107328-107337
107338-107356
[continued]
Zones Lithology
107357-107360
107361-107368 107117-107121 107122-107134 107369-107375 107376-107383
107384-107393 107394-107401 107135-107146 107147-107158
107402-107412
107483-107499 107600-107613 107614-107625
107626-107639
107640-107670107212107213
107671-107702
107703-107711
94-103 D sul3 103-121 M sul
121-132 D sul
4 132-153.6 V-S
0-28
28-392 39-61
61-74
V-S
M sul, V-S M sul D sul
74-87 D + M sul 3 87-117 M sul
4 117-129.9 D sul
1 0-35 V-S2 35-63 M sul3 63-91.5 D sul
1 0-24 V-S
24^84 M sul2
3 84-126 D + M sul
4 126-138.5 V-S
92
B. List of samples from drill holes
Depth (meters)
Area H
WS-8
0-38
39^4.3 44.3-64
44-65 70-71.4 65-74.9
74.9-87
85-87
87-95
95-121
121-152.6
Area I
WS-9
0-4141-42
42-52 44-45.5 50-51.6 52-53
67-67.8 53-128
130-141 123-129141-142142-154.4
Sample numbers
[continued]
Zones
107712-107722
107170-107174107175-107185107723-107728107186107729-107735107211107736-107744
107187-107188
107745-107799
107750-107763
107764-107787
107788-107794 107189
107190-107197 107795-107797
107198 107798-107851
107199-107210 107852-107853
107854-107863
1 0-38
38-82
82-87
3 87-95
4 95-121
5 121-135 135-152.6
1 0-42
2 42-53
3 53-128
4 128-142
5 142-154.4
Lithology
V-S
M sul
M sul, V-S
V-S
D + M sul
V-SD sul, V-S
Gossan + V-S
M sul
Diorite
M sul
Diorite
93
SAMPLE
C. ANALYSES OF CORE SAMPLES
[See page 57 for description of geochemical data]
LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-NI-P CM-MO AA-CR-T
107010107011107012107013107014
107015107016107017107018107019
107020107021107022107023107024
107025107027107028107029107030
107031107032107033107034107035
107036107037107038107039107040
107041107042107043107044107045
107046107047107048107049107050
107051107052
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 24
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E
3,00003,000012,000014,000025,0000
29,000016,000018,000018,000012,0000
18,000038,000099,0000150,000029,0000
O.OOOOB34,000028,000021,000015,0000
25,000021,000020,000049,000078,0000
70,000019,000015,000010,000014,0000
15,000017,000015,000016,000022,0000
16,0000155,000028,000014,000012,0000
13,000012,0000
33,000036,000069,000069,000043,0000
84,000069,000075,000090,000090,0000
60,000069,000069,000075,000036,0000
O.OOOOB36,000024,000069,000084,0000
84,0000110,0000126,0000110,000069,0000
75,0000117,000056,0000100,000080,0000
90,000092,0000110,0000110,000092,0000
97,000092,000092,000092,000090,0000
90.000090,0000
10,000010,000020,000019,000050,0000
45,000050,000050,000060,000045,0000
51,000030,000033,000038,000040,0000
O.OOOOB85,000077,000060,000042,0000
73,000048,000042,000045,000080,0000
80,000057,000040,000035,000030,0000
40,000029,000030,000029,000030,0000
43,000037,000032,000035,000024,0000
31,000033,0000
1,15000,90000,25000,50000,4000
0,40000,40000,40000,40000,4000
0,25000.1000N0,40000.100W0,5000
O.OOOOB0,25000,40000.1000N0,4000
0,40000,40000,50000,50000,5000
0,40000,40000,50000,70000,6000
0,40000,70000,40000,50000,4000
0,40000,40000,25000,40000,4000
0,50000,5000
50,000060,0000
223,0000195,0000200,0000
145,0000170,0000108,0000183,0000158,0000
165,0000185,0000233,0000275,000068,0000
O.OOOOB165,0000120.0000145,0000210,0000
158,0000210,0000195,0000183,0000108,0000
133,0000183,0000210,0000215,0000195,0000
210,0000250,0000210,0000275,0000250,0000
210,0000223,0000215,0000215,0000233,0000
240,0000210,0000
23,000035,000067,000041,000078,0000
67,000067,000060,000060,000060,0000
73,000067,000060,000094,000041,0000
O.OOOOB73,000060,000055,000067,0000
50,000073,000073,000064,000073,0000
87,0000100,000067,000067,000087,0000
55,000080,000060,000080,000080,0000
55,000073,000064,000064,000050,0000
67,000057,0000
20,000020,00005.0000L5.0000L5.0000L
5.0000L5.0000L5,00005.0000L5.0000L
5.0000L5.0000L5.0000L5.000015.0000L
O.OOOOB5.0000L5.0000L5.0000L5.0000L
5.0000L5,00005,00005,00005.0000L
5,000010,00005.0000L5,00005,0000
5,000010,00005,000010,00005.0000L
5.0000L5.0000L5.0000L5.0000L5.0000L
5.000015.0000L
20.0000N20.0000N20.0000N20.0000N20.0000N
20.0000N20.0000N20.0000N20.0000N20.0000N
20.0000N20.0000N20.0000N20.0000N20.0000N
O.OOOOB20.0000N20.0000N20.0000N20.0000N
20.0000N20.0000N20.0000N20.0000N20.0000N
20.0000N20.0000N20.0000N20.0000N20.0000N
20.0000N20.0000N20.0000N20.0000N20.0000N
20.0000N20.0000N20.0000N20.0000N20.0000N
20.0000N20.0000N
94
ANALYSIS OF CORE SAHPLES (CONTINUED)
SAHPLE LATITUDE LONGITUD AA-HN-P
107010 107011 107012 107013 107014
107015107016107017107018107019
107020107021107022107023107024
107025107027107028107029107030
107031107032107033107034107035
107036107037107038107039107040
107041107042107043107044107045
107046107047107048107049107050
107051107052
18 18 18 18 18
13IS181818
1818181818
1818181818
181818IS18
1818181818
1818181818
1818131818
1818
24 24 24 24 24
2424242424
2424242424
2424242424
2424242424
2424242424
2424242424
2424"sis.
24
2424
06N 06N 06N 06N06N
06N06H06N06N06N
06N06N06N06306N
Q6N06N06N06N06N
06N06N06*106N06H
06N06N06M
06Nm
06H06M06N06NOdN
m06^«%>:!W$06JI
06NWN
44 44 44 44 44
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
13 13 13 13 13
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131311
1313
16E 16E 16E 16E 16E
16E16E16E16E16E
16E16E16E16E16E
16E16E16E16E16E
16E16E16E16E16E
16E16E16E16E16E
!6E16E16E16E16E
16E16E16E16E16E
16E
8.0000 9,0000 2,0000 22,0000
560,0000
850,0000850,00001000,0000830,0000565,0000
560280242680355
0500430
,0000,0000,0000.0000,0000
,00008,0000,0000
430*0000145
680280245322970
830312192
,0000
,0000,0000,0000,0000,0000
.0000,0000,0000
182,0000155
245312312210245
150355185430375
265
,0000
,0000,0000.0000,0000,0000
,0000,0000,0000,0000,0000
,0000m 312,0000
95
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-NI-P CH-HO AA-CR-T
107057107058107059107060107061
107062107063107064107065107066
107067107068107069107070107071
107072107073107074107075107076
10707710707S107079107080107081
107082107083107084107085107086
107087107088107089107090107091
107092107093107094107095107096
107097107098
18 23 13N18 23 13N18 23 13N18 23 13N18 23 13N
18 23 13N18 23 13N18 23 13N18 23 13N18 23 13N
18 23 13N18 23 13N18 23 13N18 23 13N18 23 13N
18 23 13N18 23 13N18 23 13N18 23 13N18 23 13N
18 23 13N18 23 13N18 23 13N18 23 13N18 23 13N
18 23 13N18 23 13N18 23 13N18 23 13N18 23 13N
18 23 13N18 23 13N18 23 13N18 23 13N18 23 13N
18 23 13N18 23 13N18 23 13N18 23 13N18 23 13N
18 23 13N18 23 13N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
13 34E13 34E13 34E13 34E13 34E
13 34E13 34E13 34E13 34E13 34E
13 34E13 34E13 34E13 34E13 34E
13 34E13 34E13 34E1.3 34E13 34E
13 34E13 34E13 34E13 34E13 34E
13 34E13 34E13 34E13 34E13 34E
13 34E13 34E13 34E13 34E13 34E
13 34E13 34E13 34E13 34E13 34E
13 34E13 34E
12.000012.000012.000021.000016.0000
16.000020.000011.000014.000012.0000
34.000011.000012.000012.000012.0000
20,000014.000016.000012.000011.0000
9.000012.000012.000010.000010.0000
11.000012.000018.000014.000017,0000
15.000016.000018.000014.000015.0000
30,000029.000030.000031.000019.0000
21.000020.0000
84.000090.000080.000075.000084.0000
75.000075.000084.000092,000084.0000
50.0000100,000090,000069.000090.0000
90.000063.000075.0000117.0000110.0000
92.0000110.000097.0000100.0000117.0000
105.0000110.0000114.0000105.0000105.0000
114,0000110,0000102.000092.000090.0000
92.000090.000090.000080.0000100.0000
75.0000110,0000
16.000018.000015.000024.000020.0000
24.000024.000025.000022.000024.0000
130.000024.000032.000058.000033.0000
35.000027.000031.000031.000033.0000
27.000030.000031.000024.000029.0000
38.000040.000037.000038.000040.0000
33.000037,000038.000043.000044.0000
55,000045.000057.000058.000040.0000
64.000071.0000
0.1000N0.40000.40000.20000.1000N
0.1000N0.1000N0.1000N0.20000.1000N
0.50000.40000.20000.20000.1000N
0.1000N0.1000N0.1000N0.40000.1000N
0.40000.40000.60000.60000,3000
0.25000.45000.30000.30000.3000
0.20000.30000.20000.20000,2500
0,40000,40000,40000,40000,4500
0,40000.5000
233.0000240.0000183.0000233,0000215.0000
223,0000263,0000190,0000223,0000210.0000
73.0000223.0000190.0000150.0000210.0000
233.0000183.0000215.0000195,0000233.0000
195.0000233,0000210,0000210,0000190,0000
210,0000230.0000223.0000210.0000215.0000
210.0000190.0000233.0000170.0000145.0000
133.0000133.0000115.0000145.0000158.0000
128.0000140.0000
67.000060.000060.000067.000050.0000
48,000055.000055.000064.000048.0000
41.000057.000060.000057.000055.0000
50.000055,000067,000064,000055,0000
67,000078,000073,000057,000060,0000
64,000067,000070,000070,000073,0000
67.000055.000055.000067.000050.0000
67,000055.000055,000087,000067,0000
78,000070.0000
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L5,OOOOL5,OOOOL5.0000L
5.0000L5,OOOOL10.00005.0000L5.0000L
5.0000L5.0000L5,000010,00005.0000
5.0000L5,00005,000010,00005 ,00001
5.0000LSrOOOOL5.0000L5,OOOOL5,00001
5.0000L5,OOOOL5,OOOOL5.0000L5.0000L
5.0000L5,OOOOL
20.0000N20,0000*120.0000N20.0000N20.0000N
20.0000N20.0000M20,0000*120»OOOON20.0000M
20,OOOON20,00001120.0000N20.0000N20.0000N
20,OOOON20.0000N20.0000N20.0000H20.0000N
20.0000N20,OOOON20.0000N20.0000N20.0000N
20,OOOON20.0000N20,OOOON20.0000N20.0000N
20.0000N20.0000N20.0000N20.0000N20»OOOON
20.0000N20.0000N20.0000N20.0000N20.0000N
20*OOOON20.0000N
96
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAHPLE LATITUDE LONGITUD AA-HN-P
107057107058107059107060107041
107062107063107064107065107066
107067107068107069107070107071
107072107073107074107075107076
107077107078107079107080107081
107082107083107084107085107086
107087107088107089107090107091
107092107093107094107095107096
107097107098
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818
2323232323
2323232323
2323232323
2323232323
2323232323
2323232323
2323232323
2323232323
2323
13N13N13N13N13N
13N13N13N13N13N
13N13N13N13N13N
13N13N13N13N13N
13N13N13N13H13N
13N13N13N13N13N
13N13N13N13N13N
13N13N13N13N13N
13N13N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E
27,000050.000028,000060,000020,0000
32.000027,000065.0000122,000085,0000
700.000058.000075,0000275,000085,0000
240.0000275,0000225.0000400,0000230,0000
200,0000270,0000162.0000200,0000235.0000
280,0000230,0000115.0000180,0000130,0000
135,0000140,0000142,0000255,0000220,0000
455,0000322,0000300.0000368,0000292,0000
430,0000500,0000
97
ANALYSIS OF CORE SAHPLES (CONTINUED)
SAHPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-NI-P CH-HO AA-CR-T
107099107100107101107102107103
107104107105107106107107107108
107109107110107111107112107113
107114107115107116107117107118
107119107120107121107122107123
107124107125i07l2cio/i27107128
107129107130107131107132107133
107134107135107136107137107138
107139107140
18 2318 2318 2318 2318 23
. 18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2313 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 23
13Nmm13N13N
13N13N13N13N13N
13N13N13N13N13N
13N13N13N45N45N
45N45N45N45N45N
45N45N45N45N45N
45N45N45N45N45N
45N45N45N45N45N
45N45N
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E
38,000034,000018,000016,000014,0000
12,000012,000012,000016,000016,0000
30,000029,000018,000025,000042,0000
32,000020,000044,000019,000029,0000
80,000032,000021,000027,000022,0000
15,000024,000034,000016,000016,0000
30,000044,000026,000024,000031,0000
27,000016,000014,000029,000019,0000
18,000021,0000
117,000092,0000126,0000105,0000105,0000
131,000084,000095,0000117,0000110,0000
113,000090,0000100,0000100,000084,0000
75,000084,0000
100,000025,0000126,0000
126,000090,000097,000097,0000110,0000
110,0000110,000080,000092,000097,0000
75,000050,000069,000075,000069,0000
78,000097,000084,000092,000090,0000
84,000050,0000
60,000073,000037,000029,000031,0000
25,000025,000026,000035,000055,0000
45,000040,000026,000045,000055,0000
45,000031,000030,000021,000022,0000
28,000026,000025,000022,000026,0000
25,000028,000080,000026,000057,0000
57,000045,000045,000090,000035,0000
45,000035,000052,000068,000044,0000
45,000057,0000
0,25000,25000,40000,20000,2000
0,25000,30000,25000,25000,4000
0,40000,40000,25000,25000,2500
0,50000,25000,40001,70000,2500
0,40000,20000,20000,1000N0.1000N
0,28000.1000N0.1000N0.1000N0.1000N
0,1000N0.1000N0,1000N0.1000N0.1000N
0.1000N0,1000N0.1000N0,1000N0.1000N
0.1000N0.1000N
128,000098,0000178,0000158,0000158,0000
170,0000200,0000210,0000170,0000170,0000
108,0000165,0000233,0000165,0000158,0000
145,0000178,0000183,000028,0000
230,0000
195,0000183,0000195,0000183,0000210,0000
190,0000210,0000133,0000195,0000170,0000
128,0000145,0000183,0000170,0000210,0000
133,0000178,0000133,0000120,0000150,0000
183,0000195,0000
64,000055,000050,000070,000055,0000
67,000087,000050,000050,000057,0000
60,000060,000060,000050,000055,0000
55,000060,000064,000078,000070,0000
70,000039,000050,000048,000060,0000
60,000078,000070,000060,000064,0000
60,000073,000060,000067,000064,0000
70,000078,000060,000094,000080,0000
94,000087,0000
5,000015,OOOOL5,OOOOL5,OOOOL5.0000L
5,OOOOL5,OOOOL5,000015.0000L5.0000L
5.0000L5.0000L5*000015,OOOOL5.0000L
5,OOOOL5.0000L5,OOOOL5.0000L5,0000
10,00005,00005,OOOOL5,00005,0000
5,OOOOL5.0000L5.0000L5.0000L5.0000L
5,OOOOL5.0000L5.0000L5.0000L5.0000L
5.0000L5,OOOOL5,00005,00005,0000
10,000010,0000
20,OOOON20.0000N20,OOOON20.0000N20.0000N
20.0000N20.0000N20,OOOON20.0000N20,OOOON
20,OOOON20.0000N20.0000N20.0000N20.0000N
20.0000N20.0000N20.0000N20,0000120.0000N
20.0000N20.0000N20.000QN20.0000N20.0000N
20,OOOON20.0000N20.0000N20,OOOON20.0000N
20.0000N20.0000N20,OOOON20,OOOON20.0000N
20.0000N20.0000N20,OOOON20.0000N20.0000N
20.0000N20,OOOON
98
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LONGITUD AA-HN-P
107099107100107101107102107103
107104107105107106107107107108
107109107110107111107112107113
107114107115107116107117107118
107119107120107121107122107123
107124107125107126107127107128
107129107130107131107132107133
107134107135107136107137107138
107U9107140
18 23 13N 44 13 34E 850.000018 23 13N 44 13 34E 455.000018 23 13N 44 13 34E 250.000016 23 13N 44 13 34E 275.000018 23 13N 44 13 34E 375.0000
18 23 13N 44 13 34E 285.000018 23 13N 44 13 34E 260.000018 23 13N 44 13 34E 245.000018 23 13N 44 13 34E 275.000016 23 13N 44 13 34E 220.0000
18 23 13N 44 13 34E 680.000018 23 13N 44 13 34E 425.000018 23 13N 44 13 34E 368.000018 23 13N 44 13 34E 355.000018 23 13N 44 13 34E 430.0000
18 23 13N 44 13 34E 455.000018 23 13N 44 13 34E 255.000018 23 13N 44 13 34E 182.000018 23 45N 44 13 34E 22.000018 23 45X 44 13 34E 170.0000
18 23 45N 44 13 34E 236.000018 23 45M 44 13 34E 172.000018 23 45H 44 13 34E 205.000018 23 45N 44 13 34E 245.000018 23 45H 44 13 34E 355.0000
18 23 45N 44 13 34E 220.000018 23 45H 44 13 34E 298.000018 23 45K 44 13 34E 462.000016 23 45N 44 13 34E 172.000018 23 45N 44 13 34E 192.0000
18 23 45N 44 13 34E 322.000018 23 45H 44 13 34E 560.000018 23 45H 44 13 34E 338.000018 23 45H 44 13 34E 215.000018 23 45N 44 13 34E 325.0000
16 23 45H 44 13 34E 242.000018 23 45N 44 13 34E 125.000018 23 45H 44 13 34E 125.000018 23 45N 44 13 34E 230.000013 23 45H 44 13 34E 145.0000
13 23 4tiN 44 13 34E 135.000018 23 45N 44 13 34E 172.0000
99
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAHPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-NI-P CH-HO AA-CR-T
107141107142107143107144107145
107146107147107148107149107150
107151107152107153107154107155
107156107157107158107159107160
107161107162107163107164107165
107166107167107168107169107170
107171107172107173107174107175
107176107177107178107179107180
107181107182
18 23 45N18 23 45N18 23 45N18 23 45N18 23 45N
18 23 45N18 23 45N18 23 45N18 23 45N18 23 45N
18 23 45N18 23 45N18 23 45N18 23 45N18 23 45N
18 23 45N18 23 45N18 23 45N18 24 04N18 24 04N
18 24 04N18 24 04N18 24 04N18 24 04N18 24 04N
IS 24 04N18 24 04N18 24 04H18 24 04N18 20 21N
18 20 21N18 20 21M18 20 21N18 20 21N18 20 21N
18 20 21N18 20 21N18 20 21N18 20 21M18 20 21N
18 20 21M18 20 21N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
13 34E13 34E13 34E13 34E13 34E
13 34E13 34E13 34E13 34£13 34E
13 34E13 34E13 34E13 34E13 34E
13 34E13 34E13 34E13 34E13 34E
13 34E13 34E13 34E13 34E13 34E
13 34E13 34E13 34E13 34E12 18E
12 18E12 18E12 18E12 18E12 18E
12 18E12 18E12 18E12 18E12 18E
12 18E12 18E
14,000012,000019,0000130,000070,0000
14,00008,000011,000014,000015,0000
10,000011,000012,000014,000019,0000
11,000016,000021,000015,000029,0000
163,000060,000019,000015,000028,0000
19,000029,0000O.OOOOB0,00006
38,0000
38,000068,000060,000043,000050,0000
73,000047,000059,000043,000050,0000
43,000047,0000
53,000060,000069,000043,000072,0000
69,000072,000092,000092,0000117,0000
170,000084,000090,000075,000060,0000
60,000075,000060,000075,000084,0000
69,000092,0000100,0000110,000092,0000
69,000050,00000,000060,00006
60,0000
50,0000110,0000110,0000100,0000100,0000
92,000084,000092,000090,000075,0000
56,000075,0000
48,000033,000028,000029,000026,0000
26,000029,000026,000024,000031,0000
37,000035,000031,000042,000040,0000
42,000037,000035,000040,000045,0000
48,000037,000031,000064,000040,0000
42,000040,00000,000060,OOOOB45,0000
52,000031,000045,000058,0000110,0000
55,000048,000060,000048,000076,0000
70,000053,0000
0,1000N0.1000N0.1000N0.1000N0.1000N
0,1000N0.1000N0.1000N0,1000N0,1000N
0,1000N0,1000N0,iOOON0,1000N0,1000N
0,1000N0,14000,1000N0.1000N0.1000N
0,34000,1000N0,14000.1000N0,1000N
0,1000N0,28000,000080,OOOOB0,6500
0,50001,20000,65000,90001,5000
1,30001,45001.60000,90002,4500
2,85002,6000
170,0000170,0000195,0000150,0000195,0000
183,0000183,0000170,0000195,0000210,0000
183,0000183,0000183,0000183,0000178,0000
183,0000190,0000170,0000170,0000115,0000
223,0000195,0000165,0000190,0000223.0000
210,0000158,00000,00006O.OOOOB
170,0000
145,0000215,0000190,0000158,0000233,0000
230,0000263,0000223,0000150,0000255,0000
158,0000215,0000
100,000070,000064,000073,000055,0000
60,000057,000067,000060,000094,0000
73,000067,000080,000060,000080,0000
70,000064,000067,000073,000073,0000
145,000094,000087,000067,000087,0000
80,000080,0000O.OOOOBO.OOOOB
55,0000
55,000055,000055,000064,000073,0000
80,000090,000080,000060,0000
100,0000
78,000087,0000
10,00005.00005.00005.00005,0000
5,00005,00005,00005,000010,0000
10,00005,00005,000010,00005,0000
5,00005,00005,00005,000010,0000
5,00005,00005,00005,000010,0000
5,00005,00000,00006O.OOOOB
10,0000
5,OOOOL5<OOOOL5.0000L5.0000L5,OOOOL
5.0000L5.0000L5,OOOOL5.0000L5,OOOOL
5.0000L5.0000L
20.0000N20,OOOON20.0000N20,OOOON20,OOOON
20.0000N20.0000N20.0000N20.0000N20,OOOON
20.0000N20.0000N20.0000N20,OOOON20.0000N
20,OOOON20.0000N20.0000N20.0COON20.0000N
20.0000N20.0000N20.0000N20.0000M20.0000N
20.0000N20.0000NO.OOOOBO.OOOOB
20.0000N
20.0000N20.0000N20.0000N20.0000M20.0000N
20.0000N20.0000N20.0000N20.0000N20.0000N
20.0000N20.0000N
100
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LQNGITUD AA-MN-P
107141107142107143107144107145
107146107147107148107149107150
107151107152107153107154107155
107156107157107158107159107160
107161107162107163107164107165
107166107U7107168107169107170
107171107172107173107174107175
107176107177107178107179107180
107181107132
1818181818
1818181818
1818181818
1818181818
1818181818
1818181813
1818181818
1818181818
1818
2323232323
2323232323
2323232323
2323232424
2424242424
2424242420
2020202020
2020202020
2020
45H45N45N45N45N
45N45N45N45N45N
45N45N45N45N45N
45N45N45N04H04N
04H04N04N04N04N
04M04N04N04N21N
21N21H21M21N21N
21H21H21N21N21H
21H21N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
44
44444444
4444444444
4444
1313131313
13IS131313
1313131313
1313131313
1313131313
1313131312
1212121212
1212121212
1212
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E18E
18E18E18E18E1S£
i8E18E18E18E18E
18EiSt
120*0000130*0000192.0000215,0000100*0000
172.0000290.0000168.000082.0000
305*0000
275 ,0000275*0000342.0000183 .0000182.0000
168150155242180
43511017208105
160220
00
208
2902202705*0
290
3153482tS322265
.0000
.0000
.0000
.0000
.0000
.0000,0000,0000.0000.0000
,0000.0000.OOOOB.OOOOB,0000
.0000,0000,0000*0000,0000
.0000,0000.0000,0000,0000
322,0000318 .0000
101
ANALYSIS OF CORE SAHPLES (CONTINUED)
SAHPLE LATITUDE LQNGITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-NI-P CH-HO AA-CR-T
107183107184107185107186107187
107188107189107190107191107192
107193107194107195107196107197
107198107199107200107201107202
107203107204107205107206107207
107208107209107210107214107215
107216107217107218107219107220
107221107222107223107224107225
107226107227
18 20 21N18 20 21N18 20 21N18 20 21N18 20 21N
18 20 21M18 21 16N18 21 16N18 21 16N18 21 16N
18 21 16N18 21 16N18 21 16N18 21 16N18 21 16N
18 21 16N18 21 16N18 21 16N18 21 16N18 21 16N
18 21 16N18 21 16N18 21 16N18 21 16N18 21 16N
18 21 16N13 21 16N18 21 16N18 24 06N18 24 06N
18 24 06N18 24 06N18 24 06N18 24 06N18 24 06N
18 24 06N18 24 06N18 24 06N18 24 06N18 24 06N
18 24 06N18 24 06N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
12 18E12 18E12 18E12 18E12 18E
12 18E11 35E11 35E11 35E11 35E
11 35E11 35E11 35E11 35E11 35E
11 35E11 35E11 35E11 35E11 35E
11 35E11 35E11 35E11 35E11 35E
11 35E11 35E11 35E13 16E13 16E
13 16E13 16E13 16E13 16E13 16E
13 16E13 16E13 16E13 16E13 16E
13 16E13 16E
45.000050.000050.000047.000050.0000
65.000082.000070.000078.000061.0000
64.000065.000059.000064.000075.0000
70.000057.000050.000040.000036.0000
48.000042.000042.000050.000048.0000
50.000039.000045.000013.000015.0000
20.000025.000017,000018.000021.0000
20.000013.000023.000022.000031.0000
28.000017.0000
84.000082.000060.0000110.000060.0000
69.000036.000036.0000110.000092.0000
97,000080.000075.000084.0000100.0000
105.0000100.0000110.000092.0000
126.0000
153.000075.000069,000080,000084.0000
82.0000105.000084.000027,000027.0000
24.000024,000025,000017,000017,0000
18.000019,000079.000023.000016.0000
45.000017.0000
43.000055,000050.000066.000050.0000
63.000035.000053.000043.000035.0000
52.000063.000068.000037.000045.0000
35.000045.000048.0000135.000090.0000
50.000073.000035.000071.000053.0000
43.000055.000042.000031.000040.0000
28.000021.000027.000030.000025.0000
30.000032.000022.000043,000023.0000
132.000030.0000
2.25002.10002.25002,05001.9500
2.65003.05002.40002.80002.6000
2,60002.40002.25002.15002.6000
1.95002.40002.95002,95002.4000
2.60002,15002.95002.80002.6500
2.80002.40002,40002,10001.4000
1.50001.60001.00001.50001.3000
1,80001.60001.40001.50001.4000
1,70001,4000
190,0000195.0000215.0000158.0000170.0000
170.0000210.0000158,0000190,0000210.0000
195.0000178,0000158.0000183.0000183.0000
150.0000233.0000183.0000215.0000190.0000
223.0000145.0000195.0000195,0000223,0000
183.0000195.0000170,000025,000033.0000
37,000035,000033,000032,000030.0000
34,000032.000029.000027.000031.0000
40.000029.0000
64,000064,000064.000060.000073.0000
73.0000180.000087,000094.000067,0000
73.000080.000073.000067.000094.0000
73.000080.000084.000087,000094.0000
64.000067,000067,000090,000073,0000
60,000087,000084,000023,000023,0000
22,000021,000020.000022.000023.0000
23,000025,000020,000020,000023.0000
15,000022,0000
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L5.0000L5.0000L5.0000
5,00005,00005,00005.00005.0000
5.00005.0000L5.0000L5.0000L5.0000L
5.00005,00005.00005,00005,0000
5.000010.000010.00005.0000L5.0000L
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L5.0000L5.0000L5,00001
5.0000L5.0000L
20.0000N20.0000N20, 000 W20.0000N20.0000N
20.0000N20.0000N20.0000N20.0000N20.0000N
20.0000N20.0000N20, 000 W20.0000N20.0000N
20.0000N20.0000N20.0000N20.0000N20.0000N
20,0000*20.0000N20,0000*20.0000N20.0000N
20,0000*20.0000N20.0000ft20.0000L80.0000
20.0000L20.0000L20.0000L180.0000120,0000
120,000020.0000L85.0000170.000020.0000L
115.000020.0000L
102
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LONGITUD AA-HN-P
107183107184107185107186107187
107188107189107190107191107192
107193107194107195107196107197
107198107199107200107201107202
107203107204107205107206107207
107208107209107210107214107215
107216107217107218107219107220
107221107222107223107224107225
10722610722?
1818181818
1818181818
1818181818
18181818IS
1818181818
1818131818
1818181818
181818!818
1818
2020202020
2021212121
2121212121
2121212121
212121212i
2121212424
2424242424
2424242424
2424
21N21N21N21N21N
21N16N16N16N16N
16N16N16N16N16N
16H16H16H16N16N
16N16N16H16N16N
16N16N16N06H06N
06N06N06NW06N
06K06H06N06Nm
m06H
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444«44444
4444444444
4444
1212121212
1211111111
1111il1111
a111111n
11il11n11
ilil111313
1313131313
1313131313
1313
18E18E13E13E13E
18E35E35E35E35E
35E35E35E35E35E
35E35E35E35E35E
35E35E35E35E35E
35E35E35E16E16E
16£16£16E16E16£
16E16E16E16E16£
16E16E
455.0000278.0000375.0000255.0000462.0000
375.0000198.0000290,0000230,0000245.0000
222.0000472.0000388.000092.0000290.0000
275.0000440.0000308.0000620.0000435.0000
335,0000280.0000200.0000255.0000900.0000
680.0000560,0000620,0000533,0000653.0000
365.0000250.0000305.0000305,0000340.0000
288.0000455,0000365.0000290.0000265.0000
320,0000350,0000
103
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LONGITUO AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-NI-P CM-HO AA-CR-T
107228107229107230107231107232
107233107234107235107236107237
107238107239107240107241107242
107243107244107245107246107247
107248107249107250107251107252
107253i 0725415725510725^107257
107258107259107260107261107262
107263107264107265107266107267
107268107269
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2*13 2418 2418 24
18 2418 2418 2418 2418 24
18 24IS 24IS 2418 2418 24
18 2418 24
06N06N06N06N06N
06N06N06N06N06N
06*06*106N06N06N
06N06N06N06N06H
06N06M06N06N06N
06N06N06N06K'
06N
06H06M06N06N06N
06N06N06M06M06N
06N06H
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16£44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 I6E
44 13 16E44 13 16E
25,000020*000016,000015,000016,0000
20.000026,000045,0000100,000033,0000
22,000036.000038,000028.000037,0000
30,000039,000035,000025,000025,0000
24,000020,000032,000042,000025,0000
43.000073,000096.000022,0000102.0000
117,0000185,0000114,0000142.0000144,0000
139,0000116.0000141.0000152,0000147,0000
150,0000160,0000
25,000014,000013,000024,000034,0000
78,0000351,0000565.0000360,0000179,0000
310,0000135,000029,000030,000032,0000
24,000031,000046,000024,000019.0000
20,000038,000023,000024,000027.0000
23,000031,000020,000017,000025.0000
25,000023.000025,000024.000021.0000
25,000026,000024,000024,000021,0000
25,000020,0000
46,000022,000027.000043,0000110,0000
200,0000540,0000
1180,0000580,0000420,0000
610,0000264,000071,000063.000067.0000
40.000083.000048.000050,000044,0000
110,000019,000026.000036.000026,0000
36,000028,000018,000033,000094,0000
99,000042,000092,0000
870.000052.0000
100,000098,000074,000075,000056,0000
45,000065.0000
3.30001,50001,50001,40001,4000
1,30001,70001,60001,10001.6000
1,40001,50001,20001.20001,1000
1,40000,90001,10001,50001,1000
1,60001,40001.50001.30001,1000
1,30001,50001,40001,40001.4000
1.30001.30001,40001,30001,1000
1,20001,20001,40001,70001,5000
1,50001,3000
32,000031,000030,000027,000026,0000
30,000030,000044.000033.000030,0000
33.000050,000031,000037,000028,0000
37,000031,000036,000037,000036,0000
54,000048,000046,000048,000045,0000
46,000054,000051,000036,000051,0000
47,000070,000036,000047,000035,0000
45,000056,000051,000040,000035,0000
42.000035,0000
12,000023,000017,000018,000015,0000
17,000011,000016,000021,000018,0000
24.000041.000052,000059,000054,0000
72,000055,000030,000030,000051.0000
31,000060,0000149,0000117.0000142,0000
114.0000146,0000151,000078,000027,0000
35,000045,000040,000046,000039,0000
34,000036,000051,000044,000033,0000
46,000042,0000
5.0000L5.0000L5.0000L5,000015.0000L
5.0000L5.0000L5.0000L5.0000L5.0000L
S.OOOOL5.0000LS.OOOOLS.OOOOLS.OOOOL
S.OOOOLS.OOOOLS.OOOOLS.OOOOLS.OOOOL
S.OOOOLS.OOOOLS.OOOOLS.OOOOLS.OOOOL
S.OOOOLS.OOOOLS.OOOOLS.OOOOLS.OOOOL
S.OOOOLS.OOOOLS.OOOOLS.OOOOLS.OOOOL
S.OOOOLS.OOOOLS.OOOOLS.OOOOLS.OOOOL
S.OOOOLS.OOOOL
80,0000125,000020.0000L170.000020.0000L
20.0000L40,000095,0000125,000020.0000L
95,000045.000020.0000L75.000080,0000
90,0000105,000020.0000L20.0000L20,00001
20.0000L105,000020,0000L
675,000080,0000
110,0000280,0000445,0000235,000060,0000
20,00001215,0000105,0000100,000090,0000
50 , 000020, COM.20.0000L20.0000L80,0000
300,0000100,0000
104
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAtflE LATITUDE LONGITUD AA-MN-P
107228107229107230107231107232
10723310723410723510723610723?
107238107239107240107241107242
107243107244107245107246107247
107248107249107250107251107252
107253107254107255107256107257
107258107259107260107261107262
107263107264107265107266107267
107268107269
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818
2424242424
2424242424
2424242424
2424242424
2424242424
2424242424
2424242424
2424242424
2424
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N06N06N06N
06N06N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313
16E16E16E16E16E
16E16E16E16E16E
16E16E16E16E16E
16E16E16E16E16E
16E16E16E16E16E
16E16E16E16E16E
16E16E16E16E16E
16E16E16E16E16E
16E16E
535,0000220,0000350,0000288,0000250,0000
470,0000740,0000276,0000425,0000500*0000
625,00001365,0000650*0000650,0000550,0000
248,0000500,0000315,0000400,0000300,0000
450,0000375,0000248,0000283,0000235,0000
283,0000280,0000280,0000340,0000725,0000
910,0000382,0000550,0000750,0000575,0000
650,0000535,0000825,0000712,0000600,0000
500,0000700,0000
105
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAHPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-NI-P CH-HO AA-CR-T
107270107271107272107273107274
107275107276107277107278107279
107280107281107282107283107284
107285107286107287107288107289
107290107291107292107293107294
107295107296107297107298107299
107300107301107302107303107304
107305107306107307107308107309
107310107311
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 23
06N06H06N06N06N
06N06N06N06N06N
06H06N06N06N06N
06N06N13N13N13N
13N13Nm13N13H
13Nm13N13N13N
13N13Nm13N13N
13N13N13N13N13N
13N13N
44 13 16E44 13 16£44 13 16£44 13 16E44 13 16E
44 13 16£44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 16E44 13 16E44 13 16E
44 13 16E44 13 16E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E
151.0000113.000076,000037,000065,0000
24,0000169,0000110.000056,000093*0000
169,0000129,000015,000019,000019*0000
22,000023,000021,00009*00005*0000
8,00006,00007,000017,000026,0000
187*000092,000054,000038,000052,0000
76,000058.000096,000093,000078,0000
79,000096,000068.000078.0000
105*0000
91,000093,0000
10,OOOOL11*000019,000023,000030,0000
20,000013,000017.000023.000035.0000
23,000030.000016,000019*000016.0000
19,000030,000018,000012,000014,0000
12.000020*000013.000013,000014*0000
26,000016.000017,000020*000030.0000
30.000022.000022.000024*000056.0000
19,000041*000016.000022*000025,0000
36,000024,0000
28,000042,000068,000080,0000105,0000
50.000028.000041,000050,000087*0000
87.000074.000029,000031.000034,0000
30.000090.000047.000057,000063.0000
50.000070,000058,000054.000043.0000
140,000040,000055.000083,000048.0000
67.000066.000046.000051*000028*0000
30,000062,000021,000024,000028,0000
40,000033,0000
1*40000,90001,10001,20001,5000
1,80001.00001,00001,50001.9000
0,90001,40001*20001*20001*2000
1.20001,40000.60000*60000,5000
0.60000*60000.60000,70000*7000
1.50000*80000,90001,30001,5000
1,40001.10001,30001,40000.9000
1,20000,10000,90000.90001,1000
1.50001,3000
29.000025.000037,000043,000057,0000
33,000026,000026,000038.000050.0000
32,000050.000022,000020,000025,0000
28,000037,000010.000010,OOOOL10,OOOOL
10,OOOOL15,000010.0000L10,0000110.0000
35,000018,000025.000035.000045,0000
50,000038,000046,000036.000040.0000
40.000045.000037,000051,000060.0000
47,000070,0000
24.000023.000027,000055,000036,0000
25.000032,000045,000021,000032,0000
14.000026.000020,000018,000020,0000
23.000011.000023,000011.000010,0000
10.0000L3,000012,000012.000010,0000
37.000021,000022.000022.000012.0000
11,000043,0000
117,000083,0000371,0000
123,000094,0000128,0000122,0000126.0000
133.0000157.0000
5,OOOOL5,000015,000015,OOOOL5.0000L
5.0000L5.0000L5,000015,000015,00001
5,OOOOL5.0000L5,OOOOL5,OOOOL5,OOOOL
5,000015.0000L5,OOOOL5*OOOOL5,OOOOL
5,OOOOL5.0000L5.0000L5.0000L5.0000L
5,OOOOL5,000015.0000L5,OOOOL5.0000L
5.0000L5»OOOOL5,OOOOL5.0000L5.00001
5,OOOOL5,OOOOL5,OOOOL5.0000L5.0000L
5,OOOOL5.0000L
20.0000L80,0000
280,000080,0000
460.0000
150.0000110,0000230,0000170,000020.0000L
35,000050,0000175,0000390.0000560,0000
750,000065,0000165,0000105,000070,0000
190,0000130,000020.0000L155,000095,0000
140.0000145.0000505,0000145,000050,0000
50,0000145.0000160,0000515,0000415,0000
665,000030,0000
970,0000635,0000825,0000
750,0000195,0000
106
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LONGITUD AA-HN-P
107270 107271 107272 107273 107274
107275 107276 107277 107278107279
107280107281107282107283107284
107285107286107287107288107289
107290107291107292107293107294
107295107296107297107298107299
107300107301107302107303107304
107305107306107307107308107309
107310107311
18 18 18 18 18
18 18 18 1818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818
24 24 24 24 24
24 24 242424
2424242424
2424232323
2323232323
2323232323
2323232323
2323232323
2323
06N 06N 06N 06N 06N
06N 06N 06N 06N06N
06N06H06N06N06N
06H06N13Nm13N
13N13N13N13N13N
13N13N13N13N13N
13N13N13N13N13N
13N13N13N13N13N
13N13N
44 44 44 44 44
44 44 44 4444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
13 13 1313 13
13 13 13 1313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313
16E 16E 16E 16E 16E
16E 16E 16E 16E16E
16E16E16E16E16E
16E16E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E
425,0000 575,0000 650,0000 900,0000 1200,0000
650,0000 427,0000 625,0000 575,00001650,0000
350,0000397,0000475,0000430,0000403,0000
538,0000277,0000225350
,0000,0000
275,0000
247275
,0000,0000
410,0000375350
,0000,0000
687,00003004109001100
900
,0000,0000,0000,0000
,0000750,0000575500287
427262300392500
600500
,0000,0000,0000
,0000,0000,0000,0000,0000
,0000,0000
107
ANALYSIS OF CORE SAMPLES (CONTIMUED)
SAMPLE LATITUDE LON6ITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-HI-P CH-HO AA-CR-1
107312107313107314107315107316
107317107318107319107320107321
107322107323107324107325107326
107327107328107329107330107331
107332107333107334107335107336
107337107338107339107340107341
107342107343107344107345107346
107347107348107349107350107351
107352107353
18 2318 2318 2318 2318 23
IS 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 23IS 2318 2318 2318 23
18 2318 23
m13N13N13N13N
13N13M13N13N13N
13N13Nm13N13N
13N13N13N13N13N
13Nmm13N13N
13M13N13M13Nm
13Mi3Hmmm
mm13N13N13N
13N13N
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E
81.000083,000035,000015.000021,0000
15.000018,000088,0000120,0000112,0000
105,0000120,0000101,000083,0000105,0000
150,0000140,000055,000075,000052,0000
72,000076,000075.000071.000082,0000
78,000061.5000130.0000102,0000122,0000
79,000093,500095,000090,000093,5000
93,500069,500087,000040,0000100,0000
93,0000103,0000
21,000024,000020,000012,000016,0000
11,000011,000031,000038,000030,0000
38,000030,000041,000032,000032,0000
38,000034,000035,000040,000041,0000
30,000033,000030,000025,000036,0000
27,000026,000020*000017,500020,0000
21,500022,000020,000020,500021,0000
22,500025,000030,000030,000027,5000
23.500025,0000
50.000065,000020,000088,0000108,0000
106,0000123,000064,000072.000068*0000
70,000074,000086,000065,000087,0000
67,000061,000060,000085,000068,0000
86,000092,0000188,000097,000089,0000
77,0000222,000035,000033,000037,0000
71,000076,000077,000074,0000192,0000
113,000074,000088,000070,000086,0000
77,000071,0000
1,00001,30000,40000,30000,8000
0,40000,60000,90001,50001,3000
1,20001,20000,30001,30001,8000
2,00001,80001,50001,50001,6000
0,50001,80001,70000,50001,5000
1,80002,10001,80001,60001,8000
2,00002,20002,20002,40002,2000
2,00002,30002,30002,60002,4000
2,40002,2000
52,000065,000024,000040,000045,0000
69,000064,000061,000038,000062,0000
65,000066,000050,000078,000035,0000
38.000043,000039,000031,000031,0000
30,000026,000032,000029,000034,0000
35,000037,000049,000035,000039,0000
37,000036,000038,000039,000038,0000
42,000038,000040,000040,000042,0000
45,000044,0000
127,0000127,000055,000028,000033,0000
55,000055,000065,000045,000056,0000
70,000064,000056,000088,000076,0000
90,000084,000058,000020,000023,0000
21,000012,000018,000029,000021,0000
18,000021,000084,000029,000046,0000
21,000025,000023,000025,000022,0000
26,000022,000024,000025,000029,0000
27,000026,0000
5.0000L5,OOOOL5.0000L5.0000L5.0000L
5,OOOOL5.0000L5.0000L5,OOOOL5.00001
5,OOOOL5*OOOOL5.0000L5.0000L5.0000L
5.0000L5,OOOOL5,OOOOL5.0000L5.0000L
5.0000L5.0000L5,OOOOL5.0000L5*0000L
5.0000L5,OOOOL5,000015.0000L5.0000L
5,OOOOL5.0000L5,OQOOL5.0000L5.0000L
5.0000L5,OOOOL5.0000L5.0000L5,OOOOL
5,OOOOL5,OOOOL
720*0000600*0000240,000095,0000100,0000
20»OOOOL95,0000100,000095*0000105,0000
105,000020,OOOOL25,000060,0000125,0000
105,0000115,000085,000095,000020,OOOOL
40,000085,000095,0000110*0000100,0000
90,0000120,000095,0000115,000011.0,0000
90,0000105,000095,000090,0000105,0000
140.0000100,0000100,000095,0000105.0000
90,000090,0000
108
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LONGITUD AA-HN-P
107312107313107314107315107316
107317107318107319107320107321
107322107323107324107325107326
107327107328107329107330107331
107332107333107334107335107336
107337107338107339107340107341
107342107343107344107345107346
107347107348107349107350107351
107352107353
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818
2323232323
2323232323
2323232323
2323232323
2323232323
2323232323
2323232323
2323232323
2323
13N13N13N13H13H
13N13N13N13N13N
13H13N13N13N13H
13N13N13N13N13N
13N13K13N13N13N
13*13H13N13N13N
13N13N13N13N13N
13N13N13N13N13N
13N13H
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E
2150.00002420.0000
21.0000655.0000850.0000
435.00001150.0000151.00001000.0000858.0000
1000.00001050.0000785.0000888.00001450.0000
1150.0000700.0000460.0000950.0000830.0000
1400.00001630.00001400.00001350.0000900.0000
1250.00001000.0000625.0000440.0000550.0000
1090.00001250.00001250.00001300.00001175.0000
1260.00001200.00001500.00001150.00001200.0000
1100.00001100.0000
109
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAHPLE LATITUDE LON6ITUD AA-CU-P AA-PB-P AA-ZN-P AA-A6-P AA-CO-P AA-NI-P C«-HO AA-CR-T
107354107355107356107357107358
107359107360107361107362107363
107364107365107366107367107368
107369107370107371107372107373
107374107375107376107377107378
107379107380107381107382107383
107384107385107386107387107388
107389107390107391107392107393
107394107395
18 23IB 2318 2318 2318 23
18 2318 2318 2318 2318 23
IB 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
IB 2318 23
13N13N13N45N45N
45N45N45N45N45N
45N45N45N45N45N
45N45N45N45N45N
45N45N45N45N45N
45N45N45N45N45N
45N45N45N45N45N
45N45N45N45N45N
45N45N
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E
97,000086,0000111,000054,000077,0000
82,0000109,0000125,000017,000022,0000
27,000053,000024,000028,000058,0000
68,000074,000086,000014,0000
120,0000
118,0000116,000068,000094,0000127,0000
105,0000105,0000119,000095.000093,0000
111,000047,000022,000036,000040,0000
58,000047,000029,000035,000051,0000
37,000045,0000
24.500024,000028,000026,500031,0000
27,000029,000025,000023,000038,0000
33,000049,000048,000050,000062,0000
38,000026,000042,0000168,000034,0000
30,000032,000029,000030,000044,0000
35,000046,000048,000050,000043,0000
44,000090,000030,000040,000044,0000
23,000032,000031,000025,000030,0000
30,000021,0000
75.000078,000089,000076,000065,0000
202,000046,000036,000012,000018,0000
97,00001650,000035,000028,000025,0000
37,000053,000055,000064,000090,0000
77,000054,000058,000063.000065,0000
81,000056,000087,000060,000047,0000
64,000072,000089.000077,000067,0000
78,000074,000062,000046,000052,0000
87,000067,0000
2,40002,60002,80002,50003,0000
2,60002,80002,80002,60003,7000
1,20002,70002,80002,90002,7000
3,00000,40002,80003,00003,0000
3,00003,00003,00003,40004,0000
0,40003,40003,80000,50000,8000
1,00000,80000,20000,70001,0000
1,10002,00000,40001,10000,8000
0,70000,8000
48,000045,000050,000047,000050,0000
53,000058,000061,000038,000098,0000
45,000046,000092,0000103,000099,0000
82.000045,000054,000054,000060,0000
75,000057,000074.000061,000056,0000
37,000077.000079,000088,000080,0000
78,000050,000035,000072,000082,0000
77,000086,000035,000057,000053,0000
32,000077,0000
29,000026,000048,000042,0000
201,0000
161,0000153,0000150,000026,000070,0000
32,000017,000075,000088,000078,0000
100,000063,000052,000038,000039,0000
73,000051,000060,000051,000044,0000
45,000067,000076,000077,000070,0000
85,000031,000046,000070,000070,0000
77,000073,000036,000040,000047,0000
44,000078,0000
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L
20,000040,00005.0000L
5.0000L5,000$.5,000(15.0000LS.OOOOL
5.0000L5,OOOOL5«oom5*0000L3,00001
5.000CH.5,0000L5*000315.0000L5.0000L
5.0Q00L5,00001D.OOOOL5.0000120,0000
10,000010,00005.0000L5*0000110,0000
5*000015,0000
90,0000120,0000515,0000600,0000805,0000
400,0000375,0000235,000080,000020.0000L
20,OOOOL20.0000L20.0000L90,000020.0000L
20.0000L120,000020,0000L70*000085,0000
50,000060,000090,000075*000085.0000
110,000080,0000105,000085,000070,0000
50,000070,000020,0000L95.000020.0000L
60.000080.000020,OOOOL45,000060,0000
20,0000L20.0000L
110
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAHPLE LATITUDE LON6ITUD AA-HN-P
107354107355107356107357107358
107359107360107361107362107363
107364107365107366107367107368
107369107370107371107372107373
107374107375107376107377107378
107379107380107381107382107383
107384107385107386107387107388
107389107390107391107392107393
107394107395
18 23 13N 44 13 34E 1150.000018 23 13N 44 13 34E 1150.000018 23 13H 44 13 34E 1370.000018 23 45N 44 13 34E 450.000018 23 45N 44 13 34E 600.0000
18 23 45N 44 13 34E 350.000018 23 45N 44 13 34E 445.000018 23 45N 44 13 34E 200.000018 23 45H 44 13 34E 80.000018 23 45N 44 13 34E 16.0000
18 23 45N 44 13 34E 162.000018 23 45N 44 13 34E 410.000018 23 45H 44 13 34E 335.000018 23 45N 44 13 34E 470.000018 23 45N 44 13 34E 270.0000
18 23 45N 44 13 34E 365.000013 23 45fi 44 13 34E 550.000018 23 45H 44 13 34E 675.000018 23 45H 44 13 34E 730.000018 23 45N 44 13 34E 630.0000
18 23 45N 44 13 34E 650.000018 23 45N 44 13 34E 625.000018 23 45N 44 13 34E 688.000018 23 45N 44 13 34E 775.000018 23 45H 44 13 34E 750.0000
18 23 45N 44 13 34E 900.000018 23 45N 44 13 34E 710.000018 23 45N 44 13 34E 875.000018 23 45N 44 13 34E 595.000018 23 45N 44 13 34E 452.0000
18 23 45N 44 13 34E 645.000018 23 45N 44 13 34E 500.000018 23 45N 44 13 34E 630.000013 23 45N 44 13 34E 618.000018 23 45N 44 13 34E 673.0000
18 23 45N 44 13 34E 773.000018 23 45N 44 13 34E 775.000018 23 45N 44 13 34E 500.000013 23 45N 44 13 34E 378.000018 23 45N 44 13 34E 565.0000
18 23 45N 44 13 34E 587.000018 23 45N 44 13 34E 424,0000
111
ANALYSIS Of CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LON6ITUD AA-CU-P AA-PB-P AA-ZN-P AA-A6-P AA-CO-P AA-NI-P CH-HO l-CR-T
107396107397107398107399107400
107401107402107403107404107405
107406107407107408107409107410
107411107412107413107414107415
107416107417107418107419107420
107421107422107423107424107425
107426107427107428107429107430
107431107432107433107434107435
107436107437
18 2318 2318 23182318 23
18 2318 2318 2318 2318 23
18 2318 2318 2318 2318 23
18 2318 2318 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 241824
18 2418 2418 2418 2418 24
18 2418 24
45N45N45N45N45H
45N45N45N45N45fi
45H45N45N45fi45N
45N45N04H04N04N
04N04N04N04N04N
04N04N04N04N04N
04N04N04N04N04N
04N04N04N04N04N
04N04N
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 34E44 13 34E
44 13 34E44 13 34E44 13 34E44 13 20E44 13 20E
44 13 20E44 13 20E44 13 20E44 13 20E44 13 20E
44 13 20E44 13 20E
32,000039,000024,000063,0000104.0000
60,000060,000060,000062,000086,0000
86,000060,000067,000066,000089,0000
70.000075,0000125.000010.0000
115,0000
100.000093*000095,0000110.0000120.0000
105,000085.000085.000085,0000130,0000
110.0000130,000061,000085.000070.0000
70,000070,000085,000080,000085.0000
90.0000105.0000
33,000044,000039,000030,000030,0000
30,000030,000030,000033,000028,0000
34.000030,000027,000033,000035,0000
20.000033,000015,000015,000015.0000
110,000026.000013.000010,000015,0000
16.000020,000021,000012,000010,0000
15,000020,000028.000018.000016,0000
18,000020,000018,000015,000018.0000
20,000025 0000
62,000068,000041.000060,000072,0000
59.000026,000037,000028,000034,0000
42,000057,000025,000050,0000151,0000
27,000025.000028,000035,000028.0000
36,000055,000043.000049.000040.0000
50.000061,000056,000056.000068.0000
40.000061.000067.000044.000043,0000
42,000060.000054,000044.000056,0000
62.000066,0000
1,10000,80001,10001,50001,3000
1,1000*1,60001.10001,60001,5000
1,40001,40001,60000,80000,7000
1,30001,50001,00000,40000,3000
0.30000,30000,20000,30000,3000
0,20000,20000.40000.30000,1000
0.20000,20000,30000,20000,2000
0,20000,30000,20000,20000.3000
0,20000,3000
96,000091,000048,000062,000062,0000
65,000066,000072,000072,000074,0000
74,000073,000075,000050,000061,0000
72,000069,000063,000047,000051,0000
41,000045,000043,000040,000047,0000
26,000026,000029,000024,000022,0000
28,000029,000030,000028,000027,0000
25,000029,000030,000030,000028,0000
29,000028,0000
80,000073.000036,000034,000034,0000
57,0000107,0000140,0000142,0000129,0000
114,0000126.0000137,0000182.0000155.0000
152,0000100,0000123,0000167,0000161,0000
134.0000104,000092,000088,000085,0000
33.000031.000035.000031,000026.0000
27.000028,000013,000028,000028,0000
27.000030,000030,000032,000031,0000
31,000033,0000
5,00005,00005.0000L5.0000L5.0000L
5.0000L5.0000L5,00005,00005,0000
5,00005,000015,000015.0000L5,OOOOL
5,00005.00005,00005,OOOOL5.0000L
5,00005,000015,OOOOL5.0000L5.0000L
5,OOOOL5.0000L5.00005.0000L5.0000L
5,00005,00005.0000L5,00005.0000L
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L
65,000020.0000L35,000020.0000L20.0000L
20.0000120.0000L180,0000465.0000785.0000
20.0000L235,0000200,000020*OOOOL
205.0000
395.000065*000020.0000L185,0000505,0000
360,0000360,000055,000050, -000065.0000
20.0000L50,000020.0000L20.0000L20.0000L
20,0000120,OOOOL115,000025,000020.0000L
20,0000120,OOOOL20,0000145*000045,0000
20.04XKH.40,0000
112
ANALYSIS OF CORE SAMPLES (CONTIMUED)
SAtfLE LATITUDE LONGITUB AA-HN-P
107396107397107398107399107400
107401107402107403107404107405
107406107407107408107409107410
107411107412107413107414107415
107416107417107418107419107420
107421107422107423107424107425
107426107427107428107429107430
107431107432107433107434107435
1074J6107437
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818131818
1818181818
1818
2323232323
2323232323
2323232323
2323242424
2424242424
2424242424
2424242424
2424242424
2424
45N45N45N45N45N
45N45N45N45N45N
45N45N45H45N45N
45N45N04N04N04N
04H04N04N04N04H
04N04H04N04N04N
04N04N04N04N04N
04N04N04H04H04N
04H04H
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34E
34E34E34E34E34£
34E34E34E34E34E
34E34E34E34E34E
34E34E34E20E20E
20E20E20E20E20E
20E20E
454 .0000550.0000162 .0000
1060.0000775 ,0000
600.0000285.0000290.0000310 .0000340.0000
387231180378385
213273245445350
365249435530665
6007451030815570
550880825
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000595.0000555
700655575685
.0000
.0000
.0000
.0000
.0000690.0000
680 .0000850.0000
113
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-A6-P AA-CO-P AA-NI-P CH-HO AA-CR-T
107438107439107440107441107442
107443107444107445107446107447
107448107449107450107451107452
107453107454107455107456107457
107458107459107460107461107462
107463107464107465107466107467
107468107469107470107471107472
107473107474107475107476107477
107478107479
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 241824
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 2418 2418 2418 24
18 2418 24
04N04N04N04N04N
04N04N04N04N04N
04N04N04H04N04N
04N04N04N04N04N
04N04N04N04N04N
04N04N04N04N04N
04N04N04N04N04N
04N04N04N04N04N
04N04N
44 13 20E44 13 20E44 13 20E44 1320E44 13 20E
44 13 20E44 13 20E44 13 20E44 13 20E44 13 20E
44 13 20E44 13 20E44 13 20E44 13 20E44 13 20E
44 13 20E44 13 20E44 13 20E44 13 20E44 13 20E
44 13 20E44 13 20E44 13 20E44 13 20E44 13 20E
44 13 20£44 13 20E44 13 20E44 13 20E44 13 20E
44 13 20E44 13 20E44 1320E44 13 20E44 13 20E
44 13 20E44 13 20E44 13 20E44 13 20E44 13 20E
44 13 20E44 13 20E
75.0000115.0000100,0000115,000087.0000
105,000084,000095.0000110,0000130,0000
70,000035.000055,000039,000035.0000
42,000045.000050,000045,000010.0000
35,000035.000035,000040,000032,0000
25.000045,000045,000040,000055.0000
90,000095.000045,000030.000026,0000
35,000052,000035,000045,000040,0000
41.000050.0000
15,000016.000015.000016,000029,0000
70,000066,000071.000073.000020.0000
20,000030.000030.000046,000035,0000
46.000030,000030,000020,000025.0000
30,000028,000032,000032.000025,0000
30.000035,000035,000028,000035,0000
25,000023,000015.000018,000029.0000
23,000032,000018.000020,000020.0000
25,000018.0000
52.000041.000041,000043,000071,0000
49,000058,000076,000073,000041.0000
66.000055.000090.000065,000046.0000
70.000090.000090.0000117,000090,0000
95.000044.000077,000045,000084,0000
150.000037.000035.000060.000069.0000
50,0000850,000082,0000103.0000108.0000
108,0000146,0000115.0000103.000085,0000
95,000065,0000
0.30000,20000,10000,10001,4000
0,30000.10000.40000,30000,2000
0,30000.40000,60001,10000,8000
1,40000.40000,60000,80000,4000
0,40000,30000.50000,20001.4000
1.40000,60000.60000,90001.0000
0,60001.20000,60000.30001,4000
0.50001.40000,30000,70000.6000
1,00000.4000
25.000023.000020,000020.000025,0000
25,000026,000027,000027,000029,0000
26,000033.000036.000035,000030,0000
37,000029,000030,000041,000036,0000
29,000038,000029,000035.000037,0000
35,000038,000045,000046,000039,0000
29,000030,000029,000030,000030,0000
33,000035,000032,000035,000031,0000
30,000029,0000
30,000030.000031.000029.000010,0000
30.000029.000030,000030.000030.0000
30.000078,000080,000056.000078.0000
61.000070,000071.000062,000029,0000
46,000097,000059.000083.000025.0000
10.000076,000086.0000140,000098,0000
50,000010,000050,000028,00009,0000
30,000016.000030.000035,000031,0000
20.000035.0000
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.00005.0000L5.0000L5.0000
5.0000L5,00005.00005.00005,0000
5,000010,000020.000010.00005.0000L
5.0000L10.000010,00005,00005,0000
5,00005.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5,OOOOL
45,000020.0000L65*000070.000055.0000
45.000020*00001120*000040,000035,0000
40,000090.000030,000020.0000L45,0000
20.0000L80.000075,000050,000045,0000
130,0000150,000080,0000125.000020.0000L
20.0000L95.000035,0000
420.0000420,0000
175,000090,0000135,000095,000020.0000L
160,000065.0000110,000060.000090,0000
20.0000L145,0000
114
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAHPLE LATITUDE LONGITUD AA-WhP
107438 107439 107440 107441107442
107443107444107445107446107447
107448107449107450107451107452
107453107454107455107456107457
107458107459107460107461107462
107463107464107465107466107467
107468107469107470107471107472
107473107474107475107476107477
107478107479
18 18 18 1818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818
24 24 24 2424
2424242424
2424242424
2424242424
2424242424
2424242424
2424242424
2424242424
2424
04N 04N 04N 04H04N
04N04H04N04N04N
04H04N04N04N04N
04N04N04N04N04N
04N04N04N04N04N
04N04N04N04N04N
04N04N04M04N04N
04N04N04N04N04N
04N04N
44 4444 4444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
13 13 13 1313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313
20E 20E 20E 20E20E
20E20E20E20E20E
20E20E20E20E20E
20E20 20 20E20E
20E20E20E20E20E
20E20E20E20 20E
20E20E20E20E20E
20E20E20E20E20E
20 20£
650.0000 425.0000 450.0000 1180.0000805.0000
675.0000770.00001080.00001040.0000810.0000
930.0000380.0000765.0000354.0000250,0000
369.0000400.0000365.0000940.00001000.0000
790.0000230.0000645.0000295.00001050.0000
1225.0000185.0000285.00001100.00001200.0000
900.0000785.0000785.0000855.00001000.0000
970.00001180.00001140.00001220.0000990.0000
725.0000600.0000
115
ANALYSIS OF CORE SAHPLES (CONTINUED)
SAMPLE LATITUDE LON6ITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-NI-P CH-HO AA-CR-T
107480107481107482107483107484
107485107486107487107488107489 *
107490107491107492107493107494
107495107496107497107498107499
107600107601107602107603107604
107605107606107607107608107609
107610107611107612107613107614
107615107616107617107618107619
107620107621
18 24 04N18 24 04N18 24 04N18 20 35N18 20 35N
18 20 35N18 20 35N18 20 35N1820 35N18 20 35N
18 20 35N18 20 35N18 20 35N18 20 35N18 20 35N
18 20 35N18 20 35N18 20 35N18 20 35N18 20 35N
18 20 35N18 20 35N18 20 35N18 20 35N18 20 35N
18 20 35N18 20 35N18 20 35N18 20 35N18 20 35N
18 20 35N18 20 35N13 20 35N18 20 35N18 20 35N
18 20 35N18 20 35N18 20 35N18 20 35N18 20 35N
18 20 35N18 20 35N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
13 20E13 20E13 20E1243E1243E
12 43E1243E12 43E12 43E12 43E
12 43E12 43E12 43E12 43E12 43E
12 43E12 43E12 43E12 43E12 43E
12 43E12 43E12 43E12 43E12 43E
12 43E12 43E12 43E12 43E12 43E
12 43E12 43E12 43E12 43E12 43E
12 43E12 43E12 43E12 43E12 43E
12 43E12 43E
55,000045,000045,000095,000040,0000
38,000025,000018.000020,000015,0000
15,000025,000020,000015,000015,0000
15,000015,000020,000035,000055,0000
25,000020,000019,0000100,000087,0000
95,000035,0000140,0000140,0000140,0000
145,000085,0000
100,000090,000095,0000
84,000086,000092,0000106,000065,0000
82,000098,0000
18,000020,000020,000020,000018,0000
30,000025,000030,000028,000028,0000
25,000028,000030,000028,000035,0000
35,000033,000030,000026,000020,0000
38,000033,000038,000020,000020,0000
23,000018,000020,000023,000016,0000
20,000026,000020,000015,000015,0000
17,500018,000020,000019,000017,0000
16,000020,0000
54,000095,000080,000033,000018,0000
45,000037,000030,000033,000031,0000
34,000024,000033,000029,000029,0000
34,000026,000030,000048,000047,0000
54,000028,000026,000041,000067,0000
39,000047,000053,000045,000045,0000
30,000052,000034,000040,000035,0000
35,000037,000040,000025,000033,0000
23,000034,0000
0,30000,40000,40000,60000,3000
2,20000,60001,20000,90001,0000
0,10001,40000,30000,40002,0000
2,40000,80000,10000,40001,1000
0,70001,30002,10000,60001,4000
0,60000,70000,80000,50000,8000
0,90001,60000,80000,60000,4000
0,50000,70000,80000,70000,4000
0,50000,5000
32,000029,000030,000043,000045,0000
44,000033,000040,000031,000027,0000
29,000032,000033,000030,000037,0000
40,000030,000018,000021,000021,0000
19,000047,000035,000018,000040,0000
32,000048,000027,000039,000031,0000
35,000055,000034,000033,000044,0000
35,000032,000038,000051,000038,0000
43,000040,0000
38,000033,000048,000054,000097,0000
25,000063,000015,000068,000055,0000
52,000063,000060,000055,000023,0000
23.000056,000067,000081,000075,0000
75,000066,000044,0000160,0000119,0000
145,0000185,0000150,0000140,0000106,0000
130,0000109,0000115,0000120,0000140,0000
125,0000120,0000115,0000135,0000113,0000
120,0000116,0000
5.0000L5.0000L5,OOOOL5.0000L5.0000L
5,OOOOL5,OOOOL5,OOOOL5,OOOOL5,OOOOL
5,OOOOL5,OOOOL5,OOOOL5,OOOOL5,OOOOL
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5,OOOOL5,OOOOLS.OOOOL5,OOOOL
5.0000L5.0000L5,OOOOL5.0000L5,OOOOL
5,OOOOL5 ,000015,OOOOL5,OOOOL5,0000
5,OOOOL5,OOOOL5.0000L5,OOOOL5,OOOOL
5,OOOOL5.0000L
80,0000130,0000165,0000130,000070,0000
20,OOOOL135,000020,OOOOL30,000030,0000
495,000020,OOOOL20.0000L20,OOOOL20,OOOOL
20,OOOOL20,OOOOL20,OOOOL
235,0000215,0000
20.0000L20.0000L20,OOOOL620,0000415,0000
900,0000495,0000390,000020,OOOOL
600,0000
835,000020,OOOOL
415,0000390,0000295,0000
565,0000440,0000385,0000385,0000485,0000
20,00001205,0000
116
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LON6ITUD AA-HN-P
107480107481107482107483107484
107485107486107487107488107489
107490107491107492107493107494
107495107496107497107498107499
107600107601107602107603107604
107605107606107607107608107609
107610107611107612107613107614
107615107616107617107618107619
107620107621
1818131818
1818131818
1818181818
1818181818
1818131818
1818181818
1818181818
1818181818
1813
2424242020
2020202020
2020202020
2020202020
2020202020
2020202020
2020202020
2020202020
2020
04N04N04N35N35N
35N35N35N35N35N
35N35N35N35N35N
35N35N35N35N35N
35N35H35N35N35N
35N35N35N35N35H
35N35N35N35M35N
35N35N35H35M35N
35N35N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1313131212
1212121212
1212121212
1212121212
1212121212
1212121212
1212121212
1212121212
1212
20E20E20E43E43E
43E43E43E43E43E
43E43E43E43E43E
43E43E43E43E43E
43E43E43E43E43E
43E43E43E43E43E
43E43E43E43E43E
43£43E43E43E43E
43E43E
570.0000670.0000600.000085.000015.0000
270.0000235.0000126.0000180.000090.0000
60.000085.0000130.0000100*000070.0000
105.000025.000080.0000155.0000110.0000
250.0000325.0000435.0000410.0000740.0000
420,0000320.0000460.0000475.0000660.0000
300.0000580.0000285.0000300.0000232.0000
236.0000339.0000307.0000251.0000275.0000
276.0000314.0000
117
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-A6-P AA-CO-P AA-NI-P CM-MO AA-CR-T
107622107623107624107625107626
107627107628107629107630107631
10763210?633107634107635107636
107637107638107639107640107641
107642107643107644107645107646
107647107648107649107650107651
107652107653107654107655107656
107657107658107659107660107661
107662107663
18 2018 2018 2018 2018 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 21
35N35N35N35N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N
44 12 43E44 12 43E44 12 43E44 12 43E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E
95,000087,500080,000095,000064,0000
18,000012,500011,000015,000026,5000
34,000019,000045,000039,000022,5000
16,000052,500018,000018,000024,0000
22,000016,500031,500016,500016,5000
15,500016,000020,000025.000018.5000
14,000044,000021,500020,000034,0000
45,000050,000047,500027,500033,0000
25,000019*0000
21,000022,000030,000030,000026.0000
31,000046,000030,000029,000027,0000
30,000030.000026,500026,500031,0000
42,000040,000035,000030.000025,0000
30,000030,000030,000030,000027,5000
32,500035,000030,000030,000035,0000
40,000045,000027,500030,000030,0000
25,000030,000025,000035,000043,0000
20,000027,5000
40,000033.000035.000028.000034,0000
28,000021,000025,000023,000046,0000
35,000044,000067,000050,000034,0000
35,000055,000054,000027,000051,0000
35,000033,000054.000085,000070,0000
40,000035,000048,000038.000034,0000
27,000038,000065,000039,000043,0000
59,000062,000048,000039,000049,0000
55,000035,0000
0.60000.50000,30000,10002,7000
2,7000O.OOOON0,30000,10000,1000
0,10000,30000,60000,30000,5000
0,20000,20000,20000,20000,2000
0,10000,40000,30000,10000,1000
0,10000,20000,10000,10000,3000
0,90000,20000,20000,10000,2000
0,40000.20000,10000.10000.1000
0,10000,1000
48,000037,000039,000055,000090,0000
44,000017,000019,000017,000021,0000
22,000021,000022,000026,000021 ,0000
20,000020,000022,000018.000021,0000
19,000022,000020,000021,000021,0000
12,000023,000023,000019,000021,0000
19,000020,000022,000022,000022,0000
24,000023,000021,000022,000023,0000
23,000022,0000
150,0000115,0000131,0000155.0000210,0000
34,000073,000072,000077,000079.0000
86,000083.000071,000088,000083.0000
81,000080,000086.000088,000084,0000
88.000033,000099,000082,000079,0000
78,000083,000081,000083,000085,0000
78,000083,000075,000084,000078,0000
76,000080,000069,000073,000079,0000
65,000074,0000
5.0000L5.0000L5,00005,00005.0000L
5.0000L5,00005,00005,00005,0000
5,00005.00005.0000L5,00005,0000
5,000020,00005.0000L5,00005.0000L
5,00005.00005,00005.00005.0000
5,00005,00005.0000L5,00005,0000
5,00005,00005,00005,00005.0000L
5,00005,00005,00005.0000L5,0000
5.0000L5.0000L
475,0000475,0000320,0000360,000020.0000L
20,OOOOL20,OOOOL20.0000L20.0000L20,OOOOL
20.0000L20.0000L20.0000L20.0000L20.0000L
20.0000L20.0000L20.0000L20.0000L20.0000L
20.0000L20.0000L20,OOOOL20.0000L20.0000L
20.0000L20.0000L20.0000L20,OOOOL20.0000L
20.0000L20.0000L20.0000L20.0000L20.0000L
20.0000L20.0000L20.0000L20.0000L20.0000L
20.0000L20.0000L
US
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAHPLE LATITUDE LONGITUB AA-HN-P
107622107623107624107625107626
107627107628107629107630107631
107632107633107634107635107636
107637107638107639107640107641
107642107643107644107645107646
107647107648107649107650107651
107652107653107654107655107656
107657107658107659107660107661
107662107663
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818
2020202021
2121212121
2121212121
2121212121
2121212121
2121212121
2121212121
2121212121
2121
35N35N35N35N20N
20H20N20N20N20N
20N20N20H20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1212121213
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313
43E43E43E43E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E
202.0000265*0000185,0000190.0000165,0000
22,000016*000027,000056,0000
217,0000
388,0000398,0000850,0000315,0000394,0000
173,0000316,0000327,0000332,0000430,0000
404,0000486,0000565,0000250,0000400,0000
210,0000159,0000271,0000355,0000245,0000
279,0000289,0000425,0000330,0000260,0000
683,0000865,0000765,0000371,0000452,0000
478,0000325,0000
119
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAHPLE LATITUDE LQNGITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-NI-P CM-MO AA-CR-T
107664107665107666107667107668
107669107670107671107672107673
107674107675107676107677107678
107679107680107681107682107683
107684107685107686107687107688
107689107690107691107692107693
107694107695107696107697107698
107699107700107701107702107703
107704107705
182118 21182118 2118 21
182118 211821182118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 21
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20H20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N
44 13 03E44 1303E44 1303E44 13 03E44 1303E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 13 03E
17,500016,000038,000039,000025,0000
56,000052,500020,000030,000033,5000
26,000021,000034,000034,000048,0000
70,500070,500055,000045,000031,5000
35,000060,500063,000061,000050,0000
59,000037,500046,500061,500037,0000
59,000040,000080,000083,000040,0000
31,500031.000067,000053,500069,5000
17,500048,0000
25,000027,000024,000025,000030,0000
37,000035,000030,000025,000030,0000
35,000040,000030,000025,000020,0000
15,000015,000020,000020,000017,5000
20,000020,000020,000017,500020,0000
20,000020,000020,000020,000025,0000
25,000020,000025,000020,000015,0000
25,000025,000025,000020,000025,0000
15,000020,0000
29,000037,000058,000059,000053,0000
61,000040,000045,000084,000047,0000
34,000040,000042,000047,000056,0000
85,000085,000064,000077,000053,0000
56,000068,000079,000081,000061,0000
79,000063,000065,000083,000066,0000
65,000049,000061,0000
520,000061,0000
56,000054,000055,0000430,000058,0000
92,000076,0000
0,10000,10000,20000,20000,2000
0,10000,20000,10000,20000,1000
0,20000,60000,60000,50000,6000
0,50000,60000,50000,70000,6000
0,50000,70000,90000,60000,7000
0,60000,60000,90000,10001,1000
0,90000,80000,80001,00000,9000
1,10001,30001,00001,30001,4000
1,10001,3000
24,000024,000022,000023,000023,0000
22,000024,000024,000023,000024.0000
26,000024,000025,000026,000025,0000
25,000017,000023,000023,000024,0000
24,000030,000027,000026,000026,0000
24,000023,000027,000026,000026,0000
30,000025,000032,000023,000025,0000
29,000035.000037,000023,000021,0000
40,000023,0000
75,000073,000067,000074,000079,0000
73,000077,000073,000065,000076,0000
83,000079,000085,000083,000070,0000
64,000042,000066,000074,000067,0000
65,000063,000073,000060,000067,0000
71,000063,000065,000045,000077,0000
75,000092,000094,000080,0000124,0000
139,000091,0000132,000055,000036,0000
29,000041,0000
5,00005.0000L5,00005,00005.0000L
5.0000L5.0000L5.0000L5.0000L5,OOOOL
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5,000015.0000L5,00005,0000
5,00005.0000L5.0000L5,00005,00001
5,OOOOL5,00005,00005,00005.0000L
5,000015.0000L
20,000020.0000L20,0000120,OOOOL65,0000
20.0000L20,0000120,0000120,OOOOL20,00001
20.0000L20.0000L20,OOOOL20.0000L20,00001
155,0000125,0000100,0000100,000060,0000
90.000065,000020,OOOOL20.0000L20.0000L
60,000055,000095,000075,000020.0000L
50,0000105,000020.0000L75,000040,0000
20,OOOOL20.0000L20,0000155,000065,0000
20.0000L50,0000
120
ANALYSIS OF CORE SAHPLES (CONTINUED)
SAMPLE LATITUDE LONGITUD AA-HN-P
107664107665107666107667107668
107669107670107671107672107673
107674107675107676107677107678
107679107680107681107682107683
107684107685107686107687107688
107689107690107691107692107693
107694107695107696107697107698
107699107700107701107702107703
107704107705
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818
2121212121
2121212121
2121212121
2121212121
2121212121
2121212121
2121212121
2121212121
2121
20N20ti20N20N20N
20N20N20N20H20N
20N20N20H20N20N
20NW20N20N20N
20N20N20N20N20N
20N20N20N20N20N
20N20N20N20H20N
20N20N20N20N20N
20N20N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313131313
1313
03E03E03E03E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E03E03E03E
03E03E
213.0000310.0000640*0000568.0000465.0000
590.0000375.0000285.0000470.0000330.0000
462.0000292.0000500.0000402.0000588.0000
813.0000835.0000690.0000610.0000500.0000
451.0000675,0000715.0000740.0000635.0000
720.0000525.0000590.0000670.0000625.0000
568.0000608.0000725.0000788.0000388.0000
188.0000317.0000388.00001135.0000650.0000
390.0000563.0000
121
ANALYSIS OF CORE SAMPLES (COHTMO)
SAHPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-NI-P CK-HO AA-CR-T
107706107707107708107709107710
107711107712107713107714107715
107716107717107718107719107720
107721107722107723107724107725
107726107727107728107729107730
107731107732107733107734107735
107736107737107738107739107740
107741107742107743107744107745
107746107747
18 2118 2118 2118 2118 21
18 2118 2018 2018 2018 20
18 2018 2018 2018 2018 20
18 2018 2018 2018 2018 20
18 2018 2018 2018 2018 20
18 2018 2018 2018 2018 20
18 2018 2018 2018 2018 20
18 2018 2018 2018 2018 20
18 2018 20
20N20N20N20N20N
20N21N21N21N21N
21N21N21N21N21N
21N21N21N21N21N
21N21N21N21N21N
21N21N21N21N21N
21N21N21N21N21N
21N21N21N21N21N
21N21N
44 13 03E44 13 03E44 13 03E44 13 03E44 13 03E
44 13 03E44 12 18E44 12 18E44 12 18E44 12 18E
44 12 18E44 12 18E44 12 18E44 12 18E44 12 18E
44 12 I8E44 12 18E44 12 18E44 12 18E44 12 18E
44 12 18E44 12 18E44 12 18E44 12 18E44 12 18E
44 12 18E44 12 18E44 12 18E44 12 18E44 12 18E
44 12 18E44 12 18E44 12 18E44 12 18E44 12 18E
44 12 18E44 12 18E44 12 18E44 12 18E44 12 18E
44 12 18E44 12 18E
68,000061.000043.000055.000055.5000
50,500020,000025,000015,000028,0000
14,000022,000019,000036,000071,0000
81,000039,000037,000049,000044,0000
24,000023,000027,000019,000015,0000
22,000023,000037,000042,000045.0000
42.000051,000055.000058,000049,0000
35,000040,000018,000047.000070,0000
57,000060,0000
20.000015.000020,000020,000020,0000
25.000012.000010.0000L16,000018,0000
13,000014.000025.000017,000017.0000
22,000021,000027,000031.000029,0000
18.000019,000020,000018,000020,0000
25,000025.000025,000028,000032,0000
27,000030,000030,000035.000025.0000
25,000027,000020,000020,000016,0000
15,000015,00*?
47.000045,000044.000053.0000150.0000
51,000016,000010,000053.000050,0000
79,000060,000068,000063,000058.0000
48.000066,000038,000062.000055,0000
53.000034,000047,000046,000045.0000
62,000065,000060,000035,000074,0000
41.000046,000057,000044,000046,0000
39,000061,000062,000042,000052.0000
45,000041,0000
1,50001,10001,40001,30001.3000
1.60000,80000,60000,90000,5000
0,50000.50000.70000,50000,5000
0,80000,50000,50000,40000,3000
2,10000,40000,30000,40000,5000
0.50000.60000.60001.30000,4000
0,20000.30000,20000,30000.2000
0.20000,30000,30000,40000,7000
0,60000,4000
21.000022,000024,000025.000022.0000
28,000015,000021,000025,000025,0000
14.000025.000025,000035,000040.0000
40.000035.000055,000070.000065,0000
40.000040,000040,000035,000035,0000
60,000038.000053.000060,000068,0000
59.000060,000065.000075.000063,0000
75,000045,000030,000035,000035,0000
28,000035,0000
54.000070,000064,000074.000070,0000
141,000018,000015,000017*000021,0000
15,000017.000022.0000101,0000139.0000
89,000031,000055,000049,000049,0000
26.000024,000024,000018,000020,0000
27,000025,000032,000037,000048,0000
44,000050,000046.000059,000036.0000
33,000036,000019,000077,0000100,0000
90,000075,0000
5.0000L5,000015.000015,000015.0000L
5.0000L5,00005,00005,00005,0000
5,00005.00005.00005,00005,0000
5,00005,00005,000010,000010,0000
5,00005,00005,00005.00005,0000
5.00005,00005,00005.00005.0000
5.00005,00005,00005,00005,0000
5,00005.00005,00005.00005.0000
5,00005,0000
95,000070,000070.000095,000v95,0000
60,0000123,0000150,0000135,0000310.0000
330.000080.000080,0000215,0000310,0000
115,000030,000015,000015,000015,0000
85,000020,000070.0000100,000020,0000
105,0000130,000020,000020,000015.0000
15,000015,0000155,000015,000020,0000
15*000020,0000
220,0000305,0000270,0000
350,0000190.0000
122
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LOHGITUD AA-HN-P
107706107707107708107709107710
107711107712107713107714107715
107716107717107718107719107720
107721107722107723107724107725
107726107727107728107729107730
1077311077^2107733107734107735
107736107737107738107739107740
107741107742107743107744107745
107746107747
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818
2121212121
2120202020
2020202020
2020202020
2020202020
2020202020
2020202020
2020202020
2020
20N20N20N20N20N
20N21H21N21N21N
21N21N21N21N21N
21N21H21N21N21N
21N21N21N21N21N
21N21M21N21*21H
21N21N21N21N21N
21N21H21N21N21N
21N21N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1313131313
1312121212
1212121212
1212121212
1212121212
1212121212
1212121212
1212121212
1212
03E03E03E03E03E
03E18E18E18E18E
18E18E18E18E18E
18E18E18E18E18E
18E18E18E18E18E
18E18E18E18E18E
18E18E18E18E18E
18E18E18E18E18E
18E18E
683.0000508.0000675.0000685.0000640.0000
720.000069.0000281010
.0000,00001.OOOOL
435,0000570640550
.0000
.0000
.0000520,0000
320645590425305
420410635515450
5805901135585655
900425480330445
460655800550600
545420
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
123
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAhPLE LATITUDE LONGITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CO-P AA-NI-P CM-HO AA-CR-T
107748107749107750107751107752
107753107754107755107756107757
107758107759107760107761107762
107763107764107765107766107767
107768107769107770107771107772
107773107774107775107776107777
107778107779107730107781107782
107783107784107785107786107787
107788107789
18 20 21N18 20 21N18 20 21N18 20 21N18 20 21N
18 20 21N18 20 21N18 20 21N18 20 21NIB 20 21N
18 20 21N18 20 21N18 20 21N18 20 21N18 20 21N
18 20 21N18 20 21N18 20 21N18 20 21M18 20 21N
18 20 21N18 20 21N18 20 21N18 20 21N18 20 21N
18 20 21N18 20 21N18 20 21N18 20 21N18 20 21N
18 20 21N18 20 21N18 20 21N18 20 21N18 20 21N
18 20 21N18 20 21N18 20 21N18 20 21N18 20 21N
18 21 16N18 21 16N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
12 18E12 18E12 18E12 18E12 18E
12 18E12 18E12 18E12 18E12 18E
12 18E12 18E12 18E12 18E12 18E
12 18E12 18E12 18E12 18E12 18E
12 18E12 18E12 18E12 18E12 18E
12 18E12 18E12 18E12 18E12 18E
12 18E12 18E12 18E12 18E12 18E
12 18E12 18E12 18E12 18E12 18E
11 35E11 35E
73,000078,000045,000019,000027,0000
60,000080,000036,000034,000022,0000
18,000078,000069,000097,000048,0000
39,000068,000031.0000118,000079,0000
73,0000103,000085,000041,000036,0000
90,000054,0000134,000057,000066,0000
75,000038,000035,000091,000032,0000
46,000080,000050,000066,000035.0000
38,000036,0000
10,000015,000017,000017,000014,0000
22,000020,000018.000022.000024,0000
22,000019,000020.000022,000020,0000
19.000014,000019,000016,000017,0000
18,000020,000019.000019,000017,0000
20,000020,000020.000020,000015,0000
18,000017,000017,000024,000017,0000
15,000020,000019,000014,000014,0000
O.COOQNO.OOOON
34,000076,000065,000037,000032.0000
41.000038,000046,000055,0000139,0000
93,000068,000044,000052,000066.0000
52,000040,000075,000042,000037,0000
44,000049,000054.000078,000063.0000
47,000065,000051,000051,000051,0000
47,000045,000034,000055,000052,0000
51,000049,000041,000041,000041,0000
80,000037,0000
0,40000,60000.40000,60000,4000
0,90000,60000.80000,20000,7000
0,90000,40000,50000,60000,4000
0,40000,40000.90000,50000.5000
0.50000.70000,80000,40000,5000
0,50000,60000,40000,90000,4000
0,30000,40000,30000,30000,3000
0,40000,30000,50000.50000,6000
O.OOOONO.OOOON
38,000038,000040,000025,000030.0000
33,000030,000033,000045,000053,0000
35,000068,000060,000034,000035,0000
25,000028,000024,000025,000025,0000
25,000023,000023,000020,000018,0000
35,000028.000060,000028,000023,0000
30,000023*000035,000065,000020,0000
25,000038,000038,000020,000020,0000
25,000025,0000
92.000050,000047,000029,000033.0000
72,0000124.000065.000016,000021,0000
36.000048,000037,000054,000070,0000
186.000060,000031,0000188,0000193.0000
190,0000173.0000100,000034,000049,0000
122,0000133,0000118.0000180,000093.0000
95,000056,000031,000056,0000104,0000
124,0000105,000086,000074,000048,0000
360,0000320,0000
5.00005,00005,00005,00005,0000
5,00005,00005,00005,00005,0000
5,00005,00005,00005,00005, WOOL
5,OOOOL5,OOOOL5,OOOOL5,OOOOL5.0000L
5,OOOOL5,OOOOL5.0000L5,OOOOL5,OOOOL
5,OOOOL5.0000L5,000015.0000L5,00001
5,OOOOL5,000015,OOOOL5.0000L5,OOOOL
5,OOOOL5.0000L5,000015,OOOOLS,OOOOL
5.0000L5,00001
200,000085,000085,0000
200.0000115,0000
210,0000240.0000250,000045,000020.0000L
130,000070,000020.0000L85,000095.0000
60,0000150,0000140,0000470,0000900,0000
545,0000460,0000230,0000115,0000245,0000
340,0000545,0000200,0000110,0000135,0000
435,0000250,0000285,0000265,0000415,0000
245,0000150,0000340,0000405,0000200,0000
225,0000520,0000
124
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAMPLE LATITUDE LONGITUB AA-HN-P
107748107749107750107751107752
107753107754107755107756107757
107758107759107760107761107762
107763107764107765107766107767
107768107769107770107771107772
107773107774107775107776107777
107778107779107780107781107782
107783107784107785107786107787
107788107789
1818181818
1818181818
1818181818
1813181818
1818181818
1818181818
1818181818
1818181318
1818
2020202020
2020202020
2020202020
2020202020
2020202020
2020202020
2020202020
2020202020
2121
21N21N21N21N21N
21N21N21N21N21N
21N21N21N21N21N
21N21N21N21N21N
21N21N21N21N21N
21N21N21N21N21N
21N21N21N21N21N
21H21M21N21N21N
16N16N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1212121212
1212121212
1212121212
1212121212
1212121212
1212121212
1212121212
1212121212
1111
18E18E18E18E18E
18E18E18E18E18E
18E18E18E18E18E
18E18E18E18E18E
18E18E18E18E18£
18E18E18E18E18E
18E18E18E18E18E
18E18E18E18E18E
35E35E
320,0000135,0000585,0000470,0000320,0000
380,0000440,0000450,0000730,0000525,0000
640520475705585
425480635350375
380495540470430
395430485395380
400405435335470
425380385340450
240225
,0000,0000,0000,0000,0000
,0000,0000,0000,0000,0000
,0000,0000,0000,0000,0000
,0000,0000,0000,0000,0000
,0000,0000,0000,0000,0000
,0000,0000,0000,0000,0000
,0000,0000
125
O O
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o o o
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ANALYSIS OF CORE SAMPLES (CONTINUED)
SAHPLE LATITUDE LONGITUD AA-HN-P
107790107791107792107793107794
107795107796107797107798107799
107800107801107802107803107804
107805107806107807107808107809
107810107811107812107813107814
107815107816107817107818107819
107820107821107822107823107824
107325107826107827107828107829
107830107831
1818181818
1818181818
1818181818
1818181818
1818181818
1813181818
1818181818
1818181813
1818
2121212121
2121212121
2121212121
2121212121
2121212121
2121212121
2121212121
2!2121rjj
21
2121
16N16N16N16N16N
16Nm16Nm16N
16NUN16N16NUN
m16N16N16NUN
16NUN16NUN16N
16NUNUN16NUN
UNUNUNUN16N
UN16NUN16N16N
16N16N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1111111111
1111111111
1111111111
1111111111
1111111111
1111111111
1111111111
1111111111
1111
35E35E35E35E35E
35E35E35E35E35E
35E35E35E35E3SE
3SE35E35E35E35E
35E35E35E35E35E
35E35E35E35E35E
35E35E35E35E35E
35E35E35E35E35E
35E35E
200.0000353.0000288.0000490.0000440.0000
675.0000755216725
.0000
.0000
.00004125.0000
4003303952981070
420445
.0000
.0000
.0000
.0000
.0000
.0000
.0000420.0000460485
520560565625241
184268460420430
385280265210300
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
370.0000388.0000230305420
640445
.0000
.0000
.0000
.0000
.0000
127
ANALYSIS OF CORE SAMPLES (CONTINUE../
SAHPLE LATITUDE LON6ITUD AA-CU-P AA-PB-P AA-ZN-P AA-AG-P AA-CQ-P AA-NI-P CH-HO AA-CR-T
107832107833107834107835107836
107837107838107839107840107841
107842107843107844107845107846
107847107848107849107850107851
107852107853107854107855107856
107857107858107859107860107861
107862107863
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 2118 2118 2118 21
18 2118 21
16N16N16N16N16N
16N16N16N16N16N
16N16N16N16N16N
16N16N16N16N16N
16N16N16N16N16N
16N16N16N16N16N
16N16N
44 11 35E44 11 35E44 11 35E44 11 35E44 11 35E
44 11 35E44 11 35E44 11 35E44 11 35E44 11 35E
44 11 35E44 11 35E44 11 35E44 11 35E44 11 35E
44 11 35E44 11 35E44 11 35E44 11 35E44 11 35E
44 11 35E44 11 35E44 11 35E44 11 35E44 11 35E
44 11 35E44 11 35E44 11 35E44 11 35E44 11 35E
44 11 35E44 11 35E
120,0000114,000065,000020,000015,0000
14,000035,000070,000040,000034,0000
25,000029,000028,000014,00009,0000
12,000012,000011*000014,000031,0000
22,000023,000060,0000151,000088,0000
76,0000106,000070,000099,0000102,0000
110,000066,0000
15,0000O.OOOON15,000050,000025,0000
30,000020,000035,000030,000035,0000
30,000030,000030,000020,000020,0000
35,000015,0000O.OOOON10,00000,OOOON
15,000010,0000O.OOOON15,000020,0000
10,000025,000015,000015,000015,0000
15,000020,0000
30,000039,000055,0000128,000063,0000
77,000032,000035,000037,000047,0000
94,000046,000060,000033,000049,0000
140,000050,000034,000036,000053,0000
22,000049,000037,000041,000048.0000
26,000029,000022,000024,000028,0000
24,000030,0000
0,40000,60000,50000,40000,4000
0,80000,30001,50001,40001,2000
1,30001,10000,80000,60001,2000
0,90000,30000,20000,20000,3000
1,00000,50000,10000,40000,3000
0,70000,70000,30000,50000,5000
0,30000,4000
30,000034,000030,000020,000020,0000
23,000025,000035,000034,000041,0000
30,000023,000025,000018,000020,0000
20,000016,000012,000013,000019,0000
33,000026,000026,000032,000024,0000
27,000026,000020,000028,000031,0000
26,000030,0000
90,000086,000053,000016,000018,0000
24,000077,0000180,0000160,0000200,0000
62,000028,000035,000022,000030,0000
28,000015,000012,000013,000021,0000
51,000043,0000160,0000170,0000175,0000
195,0000200,0000165,0000225,0000205,0000
190,0000185,0000
5,OOOOL5.0000L5*OOOOL5.0000L5,OOOOL
5.0000L5,000015.0000L5,OOOOL5.0000L
5.0000L5,OOOOL5.0000L5,OOOOL5.0000L
5.0000L5,OOOOL5.0000L5.0000L5.0000L
5,OOOOL5.0000L5,000015,OOOOL5.0000L
5.0000L5.0000L5.0000L5.0000L5.0000L
5.0000L5.0000L
395,0000860,000020.0000L
215,0000800,0000
155,0000280,0000565,0000715.000020,00001
620,000020,00001
455,0000325,0000260,0000
430,0000275,0000415*0000295*0000105,0000
265,0000780,0000615,0000385,0000550,0000
1040,0000565,0000625,0000980,0000695,0000
705,0000565,0000
128
ANALYSIS OF CORE SAMPLES (CONTINUED)
SAHPLE LATITUDE LONGITUD AA-HN-P
107832107833107834107835107836
107837107838107839107840107841
107842107843107844107845107846
107847107848107849107850107851
107852107853107854107855107856
107857107858107859107860107861
107862107863
1818181818
1818181818
1818181818
1818181818
1818181818
1818181818
1818
2121212121
2121212121
2121212121
2121212121
2121212121
2121212121
2121
16N16N16N16N16N
16N16N16N16N16N
16N16N16N16N16N
16N16N16N16N16N
16N16N16N16N16N
m16Nm16N16N
UN16N
4444444444
4444444444
4444444444
4444444444
4444444444
4444444444
4444
1111111111
1111111111
1111111111
1111111111
1111111111
1111111111
1111
35E35E35E35E35E
35E35E35E35E35E
35E35E35E35E35E
35E35E35E35E35E
35E35E35E35E35E
35E35E35E35E35E
35E35E
430*0000605.0000535.0000325,0000520,0000
585,0000480,0000950,00001360,0000885,0000
1550,0000705,0000
1045*0000605,0000965,0000
815,0000435,0000265,0000343,0000680,0000
635,0000975,0000205,0000315,0000235,0000
310,0000305,0000213,0000215,0000225,0000
250,0000230,0000
129