by byron r. berger, jan l. van der voort, david f. …carbonate rocks, and (2) a later...
TRANSCRIPT
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY
GEOCHEMICAL EXPLORATION STUDIES IN THE
DILLON, MONTANA-IDAHO 1° x 2° QUADRANGLE:
GEOCHEMICAL RECONNAISSANCE OF MINING DISTRICTS
IN THE SOUTHERN PIONEER MOUNTAINS AND VICINITY,
BEAVERHEAD COUNTY, MONTANA
By Byron R. Berger, Jan L. Van der Voort,
David F. Siems, and Eric P. We!sen
Open-File Report 79-1426
1979
CONTENTS
Page
Introduction 1
Sampling and analytical procedures 3
Bannack mining district 3
Geology 4
Mineralization 6
Geochemistry 7
Blue Wing mining district 9
Geology 9
Mineralization 11
Geochemistry 12
Ermont mining district 12
Mineralization 15
Geochemistry 16
Argenta mining district 18
Geology 18
Mineralization 20
Geochemistry 21
Baldy Mountain mining district 21
Geology 21
Mineralization 23
Geochemistry 25
Discussion 25
Results of chemical analyses 28
_ _ _ ____ _ ______________ ___________________._______ « __ /I /I~ >
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY
GEOCHEMICAL EXPLORATION STUDIES IN THE
DILLON, MONTANA-IDAHO 1° x 2° QUADRANGLE:
GEOCHEMICAL RECONNAISSANCE OF MINING DISTRICTS
IN THE SOUTHERN PIONEER MOUNTAINS AND VICINITY,
BEAVERHEAD COUNTY, MONTANA
By Byron R. Berger, Jan L. Van der Voort,
David F. Siems, and Eric P. We!sen
Open-File Report 79-1426
1979
CONTENTS
Page
Introduction 1
Sampling and analytical procedures 3
Bannack mining district 3
Geology -- 4
Mineral ization- - -- 6
Geochemistry- 7
Blue Wing mining district 9
Geology---- -- __________ __ 9
Mineral ization-- - 11
Geochemistry - 12
Ermont mining district - 12
Geologyr 12
Mineralization 15
Geochemistry 16
Argenta mining district-- -- 18
Geology 18
Mineralization 20
Geochemistry 21
Baldy Mountain mining district 21
Geology 21
Mineral ization-- 23
Geochemistry 25
Discussion-- - 25
Results of chemical analyses -- -- 28
References 44
CONTENTS continued
TABLESPage
Table 1. Trace elements in ores in the Bannack mining district 8
2. Trace elements in ores in the Blue Wing mining district 13
3. Trace elements in ores in the Ermont mining district 17
4. Trace elements in ores in the Argenta mining district 22
5. Trace elements in ores in the Baldy Mountain
mining district - 26
6. Analytical data from rock samples collected in mining
districts in the southern Pioneer Mountains,
Beaverhead County, Montana 29
7. Longitude and latitude for samples collected in mining
districts in the southern Pioneer Mountains,
Beaverhead County, Montana 41
FIGURES
Figure 1. Major mining districts in the southern Pioneer Mountains
and vicinity 2
2. Generalized geologic map of the Bannack mining district 5
3. Generalized geologic map of the Blue Wing mining
district (from Lowell/1965) 10
4. Generalized geologic map of the Ermont mining district
(from Myers, 1952) 14
5. Generalized geologic map of the Argenta mining district--- 19
6. Preliminary geologic map of the Baldy Mountain mining
district (D. R. Zimbelman, Aug. 1979, unpublished data)- 24
INTRODUCTION
Mineral resource studies are being undertaken in the Dillon, Montana-Idaho,
1° x 2° quadrangle as part of the Conterminous United States Mineral Assessment
Program (CUSMAP) of the U.S. Geological Survey. A broad spectrum of coordinated
geologic, geochemical, and geophysical data is being systematically collected
for the purposes of disseminating and interpreting mineral-resource information
for land-use planning and resource management. The synthesis of regional
geological information is an integral part of the program in order to increase
the understanding of crustal evolution and the controls on the distribution of
mineral deposits.
The overall objectives of the geochemical exploration investigations in
the Dillon project area are to (1) define the broad, regional geochemical
patterns; (2) geochemically characterize the different types of known mineral
deposits; (3) undertake research to develop and (or) evaluate regional
geochemical exploration techniques; (4) research the genesis of geochemical
dispersion patterns germane to gaining an understanding of regional metallo-
genesis and the geological controls of mineral occurrences; and (5) to provide
supportive data to the consanguineous geologic and geophysical studies.
The purpose of this preliminary report is to present reconnaissance
geochemical exploration data from mineral districts in the vicinity of the
southern Pioneer Mountains, Beaverhead County, MT (fig. 1). A considerable
number of historically productive mineral deposits occur in the southern
Pioneer Mountains, including the Bannack, Blue Wing, and Argenta mining
districts. The economically most important metals in the area discussed in
this report include silver, gold, copper, lead, zinc, and tungsten.
1
FIGURE 1.--Major mining districts in the southern Pioneer Mountains and vicinity.
Previous studies in the area have catalogued the geology, mineralogy, and
production of the various mineral deposits (Winchell, 1914; Shenon, 1931; Geach,
1972), but none of the studies have geochemically characterized the deposits in
order to build a systematic picture of the interrelationships (or lack thereof)
of the deposits for exploration and evaluation purposes. The geochemical survey
described here has found distinct elemental suites that are of considerable value
in gaining an understanding of the known deposits and, when utilized in conjunction
with other geological factors, affords one the opportunity of defining and
assessing minerals exploration targets.
SAMPLING AND ANALYTICAL PROCEDURES
Rock samples were collected during this study from selected mines and prospects
in all of the major mining districts in the vicinity of the southern Pioneer
Mountains. The samples were chosen whenever possible to represent ore, altered
host rock, and unaltered host rock. All samples were analyzed for 31 elements
using a six-step semiquantitative emission spectrographic technique (Grimes and
Marranzino, 1968), and for five elements (zinc, arsenic, antimony, tin, and
tungsten) using wet-chemical techniques. Colorimetric techniques were used to
analyze for arsenic (Almond, 1953) and tungsten (Quin and Brooks, 1972). Atomic-
absorption spectrophotometric techniques were used to analyze for zinc (Ward and
others, 1969), antimony (Welsch and Chao, 1975), and tin (Welsch and Chao, 1976).
BANNACK MINING DISTRICT
The Banncak mining district is in' T. 8 S., R. 11 W., approximately 20 miles
southwest of Dillon, MT (fig. 1). From 1862 intermittently until World War II,
Tertiary to Holocene placer deposits along Grasshopper Creek and adjacent lode
deposits were mined for the contained gold values. Shenon (1931) estimated that
approximately $10 million in placer gold and $2 million incombined metal values from
lode deposits were recovered from the district. Lyden (1948) estimated that from
3
$2-3 million in placer gold were mined. The settlement of Bannack served as the
first Montana territorial capital in 1863, and the town is now partially
restored as a state park.
Geology
The general geology of the district (fig. 2) was mapped by Lowell (1965).
Mississippian carbonates and Pennsylvanian quartzites are the oldest exposed
rocks in the district, although Precambrian metamorphic rocks and older Paleozoic
formations occur south of Bannack. Probable Laramide (L, W. Snee, Aug. 1979,
unpublished data) extrusive and intrusive rocks occupy the eastern part of the
district, and the mineral deposits in the area appear to be genetically related
to these rocks, Nonmarine Tertiary sediments and volcanic rocks are prevalent
in the area, particularly in the western part of the district.
Lowell (1965) assigned the Mississippian carbonate rocks to the Madison
Group. He recognized both the Lodgepole and Mission Canyon Limestones, although
the two formations are undivided wherever altered to marble by the intrusive
rocks, Shenon (1931) described several hundred feet of carbonate rocks in the
district consisting of blue-gray, blue-white, and pink crystalline limestone,
Some parts of the section contain abundant fossil remains, and black chert
lenses and nodules occur in the middle part of the section.
The Quadrant Quartzite crops out on the south side of the district and
consists of white to pinkish-white vitreous quartzite (Shenon, 1931).
Extrusive volcanic rocks are prevalent in the district and consist of
rhyodacite to andesite flows, tuffs, agglomerates, and tuff breccias. The
volcanic rocks are intruded by a medium-grained granodiorite stock that is
exposed at two localities in the main part of the Bannack district. The
mineralogy of the intrusion and that of the majority of the extrusive rocks
FIGURE 2.--Generalized geologic map of the Bannack mining district
nyoo 1
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tim
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fitU.lt
consists of plagioclase (andesine), orthoclase, biotite, hornblende, quartz,
and magnetite. Pyrite is common along fractures and joints (Shenon, 1931).
The age of these igneous rocks is unknown, although we infer a Laramide age on
the basis of regional geochemical and igneous patterns.
The structural framework of the area is dominated by north-trending folds
and faults. North-trending, west-dipping thrust faults bring the Madison Group
limestones over older Paleozoic carbonate rocks. The low-angle faults are
displaced by northwest- and northeast-trending high-angle structures, and all
of these faults are intruded by the granodiorite.
Mineralization
Two episodes of metallization were recognized during the present study:
(1) an early contact metasomatic event producing skarn assemblages in the
carbonate rocks, and (2) a later fracture-controlled mineralization episode.
There are two types of skarn assemblages that were recognized during the
field study: magnetite-dominant calc-silicate assemblages and garnet-dominant
assemblages, The magnetite rock occurs as pods and stringers in the Madison
limestones immediately adjacent to the granodiorite contact. Epidote,
tremolite, quartz, specular hematite, and pyrite are common accessory minerals,
although most of the exposed rocks are oxidized, and the magnetite is mixed
with serpentine, quartz, malachite, and various clay minerals. The garnet
skarn consists primarily of red garnet, pyroxene, epidote, idocrase, quartz,
calcite, and pyrite. Away from the 1imestone-granodiorite contact the limestones
are bleached and recrystallized to coarse calcite.
The vein systems crosscut the calc-silicate rocks in many instances, and
the main alteration phases associated with the veins are quartz, sericite, clay
minerals, and chlorite. The width of alteration selvages on the veins varies
from a few inches to several feet. The vein sulfides occur as open-space
fillings in quartz. The immediate edges of the veins consist of quartz and
sericite, grading outward in the larger veins into an argil!ic assemblage.
Many of the mineral deposits occur near the contact of the granodiorite and the
sedimentary rocks (Shenon, 1931), and some of the primary mineral phases in the
granodiorite are altered. Cloudy feldspar grains are common due to white mica
and clay, and biotite and hornblende are frequently altered to chlorite,
magnetite, and, less commonly, epidote. Shenon (1931) described the alteration
of hornblende to biotite, but this relationship was not confirmed during the
present investigation.
Gold is the most important ore mineral in the Bannack district. Shenon
(1931) noted the presence also of native silver, tetradymite, galena, sphalerite,
argentite, and chalcopyrite.
Geochemistry
Geochemical sampling in the district suggests that the predominant
elemental suite is gold, silver, copper, molybdenum, tungsten, and zinc
(table 1). Arsenic, antimony, and tin are also present in some of the sampled
occurrences, but the variability in 'these elements suggests that they do not
serve as useful characterizes of precious-metal mineralization. Lead was not
found to be abundant in any of the samples analyzed.
TABLE 1, Trace elements in ores in the Bannaek mining district.
Mine/prospect
Pioneer mine
Golden Leaf mine
Hillside placer
Priscilla mine
Location
Sec.
Sec.
Sec.
Sec.
8
8
8
8
Trace-element suite
Au-Ag-Cu-Mo-Sn-Zn
Au-Ag-As-Cu-Mo-Pb-W
Au-Ag-Cu-Mo-W-Zn
Ag-Cu-Mo-Sn-W-Zn
Iron and manganese oxides are the most consistent carriers of the
ore-suite elements. The garnet skarn rocks do not appear to contain the same
trace elements as the quartz veins. Magnetite skarn contains copper, silver,
and tin; adjacent to the quartz veins these rocks are highly anomalous in
silver, copper, tin, tungsten, and zinc, and are slightly anomalous in arsenic
and antimony, The altered, granodiorite does not consistently contain any of
the ore-suite elements, although copper, molybdenum, and silver are common.
The recrystallized and bleached limestone contains only trace amounts of
antimony and silver, A pervasively altered volcanic rock contains anomalous
beryllium, lanthanum, and molybdenum with minor amounts of arsenic and antimony,
BLUE WING MINING DISTRICT
The Blue Wing mining district is immediately north of the Bannack district
In T, 7 S., R. 11 W. The first locations in the district were apparently in
1864 and were the first silver deposits located in Montana (Shenon, 1931),
Total mineral production from the district is not accurately known, although
sporadic production to date of primarily silver areas has been approximately
$2*3 million (Shenon, 1931; Geach, 1972).
Geology
As in the Bannack district, Lowell (1965) found Mississippian carbonate
rocks to be the oldest rocks in the district (fig. 3), These rocks are in
tectonic contact with Laramide(?) extrusive volcanic rocks, and both of these
sequences are intruded by granodiorite.
The west-dipping Madison limestones are thrust over the Devonian Jefferson
Dolomite(?) along a northerly trend. The granodiorite is primarily but not
exclusively exposed along this thrust contact. Regional aeromagnetic data
(U,S, Geological Survey, 1975) and data from mine workings in the district
FIGURE 3. Generalized geologic map of the Blue Wing mining district (from Lowell, 1965).
(
X. \\
'"
V
\v (
!/
Ta
f* ?0
^ /'
Palfoj<>«~ Pe/ecxoic,
(fas
10
(Shenon, 1931) suggest that erosion along the fault trend has served to expose
the intrusion, but the emplacement of the intrusion was not controlled by the
thrust faulting.
Mineralization
Three types of metallization were recognized in the district during the
present study: (1) an early contact-metasomatic episode producing skarn
assemblages in the carbonate rocks, and (2) a later fracture-controlled
mineralization that produced open-space filling veins and pervasive replacement
of the limestone adjacent to the fissures.
Only garnet skarn was found in the district during this study. In addition
to garnet, pyroxene, idocrase, epidote, quartz, and calcite make up the skarn
rock,
The open-space filling veins are made up of sulfide minerals in a matrix
of quartz, calcite, and sericite. The replacement veins are made up chiefly
of dense fine-grained quartz. Alteration haloes adjacent to the open-space
fissure veins are narrow and end abruptly against ostensibly unaltered limestone
The replacement veins on the other hand have broad alteration haloes consisting
of quartz and calcite in the carbonate rocks, and quartz, calcite, sericite,
and clay in the volcanic rocks.
Shenon (1931) reported the ore minerals to consist of galena, tetrahedrite,
jamesonite, sphalerite, pyrite, chalcopyrite, argentite, cerargyrite,
pyrargyrite, polybasite, and stibnite.
The mineral deposits in the Blue Wing district are not as deeply weathered
as those in the Bannack district. Relict sulfide minerals are commonly found
in the gossans. Minerals common in the oxidized rock include quartz, goethite,
hematite, jarosite, undifferentiated iron and manganese oxides, azurite,
malachite, hemimorphite, and anglesite.
11
Geochemistry
Geochemical sampling in the district suggests that the predominant
elemental suite is silver, arsenic, cadmium, copper, molybdenum, lead, antimony,
and zinc (table 2). Tin is ubiquitous in the southern part of the district,
vanadium seems to predominate in the central part of the district, and barium
occurs in the ores of the northern part of the district.
Iron and manganese oxides give the best indications of fissure-vein
mineralization. Where the replacement deposits occur, silver, lead, antimony,
and zinc are dispersed into the alteration haloes away from the main zone of
metallization. The recrystallized and bleached limestone contains silver.
The slightly to strongly altered granodiorite contains small amounts of silver,
zinc, and antimony.
ERMONT MINING DISTRICT
The Ermont mining district and adjacent Badger Pass region are about 14
miles west of Dill on, MT, in T. 6 S., R. 11 W. The Ermont gold deposits were
discovered in 1926 (Shenon, 1931), and produced bullion until World War II
(Geach, 1972), In excess of $1,400,000 in gold (Geach, 1972) was taken from
the district, No documented production has occurred in the Badger Pass area.
Geology
The general geology of the district was mapped by Kelly (1941) and Myers
(_1952)(fig. 4), Cambrian through Mississippian sedimentary rocks are exposed
In the district, with the majority of the productive horizons occurring in
Devonian dolomites, The rocks in general strike northeast and dip to the
southeast, Andesite dikes intrude the sedimentary rocks throughout the area.
12
TABLE 2,-~Trace elements in ores in the Blue Wing mining district.
Mine/prospect
Charter Oak mine
Bob Ingersoll mine
Logan mine
Iron Mask mine
Pomeroy mine
Del Monte mine
New Departure mine
Location
Sec.
Sec.
Sec.
Sec.
Sec.
Sec.
Sec.
4
4
33
28
28
28
26
Trace-element suite
Ag-As-Cd-Cu-Mo-Pb-Sb-Sn-Zn
Ag-As-Cd-Cu-Mo-Pb-Sb-Sn-Zn
Ag-As-Cd-Cu-Mo-Pb-Sb-Sn-Zn
Ag-As-Cd-Cu-Mo-Pb-Sb-Sn-V-Zn
Au-Ag-As-Cu-Mo-Pb-Sb-V-Zn
Ag-Ba-Cd-Cu-Pb-Sb-Zn
Ag-As-Ba-Cd-Cu-Mo-Pb-Sb-Zn
13
FIGURE 4.--Generalized geologic map of the Ermont mining district(from Myers, 1952).
Ta
ic Je&rt&n
14
Northeast of the main part of the district the Cambrian Flathead
Quartzite, Wolsey Shale, and Pilgrim Dolomite crop out. Neither the Meagher
Formation, Park Shale, nor Red Lion Formation were separately recognized by
Myers (1952) in the area. The Pilgrim Dolomite crops out in the western part
of the mineralized area and consists of thick-bedded, sugary dolomite containing
some chert beds. The Devonian Jefferson Dolomite overlies the Cambrian units
and consists of thin- to medium-bedded, black, fetid dolomite. The Three Forks
Shale overlies the Jefferson and is mostly thinly laminated, fissile shale,
The Mississippian Madison Group crops out in the south and southeastern parts
of the district and hosts mineralization in the Badger Pass region.
Northerly trending andesite dikes and sills crop out in the main part of
the district and are spatially associated with mineralization. The dikes
contain andesine phenocrysts in a finer grained andesine, orthoclase, and
augite-bearing groundmass (Kelly, 1941).
The predominant structural framework of the area consists of north- to
northwest-trending high-angle faults. A major zone of thrust faulting is
exposed about 1 mile southeast of the center of the Ermont district, and this
zone transects the Badger Pass region.
Mineralization
Two distinct types of metallization can be recognized geochemically in
the district: (1) replacement gold 'deposits similar to the Carlin-type, and
(2) gold- and silver-bearing base-metal sulfide fissure veins. Only the former
type of metallization has been productive.
15
The gold ore is disseminated and occurs as replacements of limy dolomite
and also as replacements of andesite. Pyrite is the principal sulfide mineral
present, although stibnite is not uncommon. The gold does not occur as visible
particles (Kelly, 1941). Alteration in the dolomite consists chiefly of quartz
and appears to be fault controlled. Alteration in the andesite dikes consists
of quartz, sericite, kaolinite, chlorite, and calcite (Kelly, 1941).
The precious- and base-metal mineralization spatially overlaps the gold
mineralization on the western side of the Ermont district, and possibly extends
into the Badger Pass region. The mineralized samples observed were thoroughly
oxidized, but the porous nature of the silica boxworks suggests that the deposits
were formed by open-space filling. Quartz, sericite, and clay occur in the
host rocks adjacent to the veins.
Geochemistry
Geochemical sampling in the district suggests two different trace-element
suites (table 3), The main elements accompanying gold mineralization are
arsenic, barium, molybdenum, antimony, and tungsten with minor amounts of
silver, lead, and zinc. The main elements accompanying the silver minerali
zation are arsenic, cadmium, copper, molybdenum, lead, antimony, and zinc with
minor amounts of gold.
The trace elements accompanying the gold mineralization display a broad
dissemination into the bedrock around the structures controlling the
mineralization. Silicified ledges of Jefferson Dolomite and altered andesite
show the same trace-element suites. In contrast, the alteration haloes
accompanying the silver mineralization do not display the trace-element suite
except immediately adjacent to the vein. Ostensibly unaltered Jefferson
Dolomite and andesite porphyry within the district but away from the exploited
deposits do not contain elemental suites suggestive of either type of metalli
zation, although the dolomite contains anomalous amounts of silver, lead, and
antimony. __I D
TABLE 3. Trace elements in ores in the Ermont mining district.
[Parentheses () denote those elements not consistently found in all samples taken from a given deposit.]
Mine/prospect Location Trace-element suite
Gold deposits:
Ermont No. 2 Sec. 35 Au-(Ag)-As-Ba-Mo-Sb
Ermont No, 19 Sec. 35 Au-(Ag)-As-Ba-(Pb)-Sb-(Zn)
Badger mine Sec. 26 Au-(Ag)-Ba-Mo-(Pb)-Sb-W
Prospect Sec. 26 Au-(Ag)-As-Ba-Mo-(Pb)-Sb-W-(Zn)
Prospect Sec. 35 Au-(Ag)-As-Ba-Mo-Sb-(Zn)
Silver deposits:
Big West mine Sec. 35 Ag-As-Cd-Cu-Mo-Pb-Sb-Zn
17
ARGENTA MINING DISTRICT
The Argenta mining district is in T. 6 S., R. 11 W. about 1 mile north and
northeast of the Ermont district. The district extends more than 4 miles
northwest of the Argenta townsite, and as such is one of the largest precious-
and base-metal camps in the region. Ore was discovered in 1865, and production
has occurred sporadically until the present. Total production from the
district has been on the order of $6 million (Shenon, 1931; Geach, 1972)-, the
principal economic metals are gold, silver, copper, lead, and zinc.
Geology
Rocks of all ages occur in the district, but the principal mineral deposits
occur in Precambrian and Paleozoic sedimentary rocks (fig. 5). The district is
on the eastern flank of a large anticline, the core of which consists of
Precambrian quartzite. Myers (1952) called this prominent structural feature
the Humboldt Mountain anticline.
The northwestern part of the district consists primarily of complexly
faulted Precambrian and Cambrian quartzite, shale, and dolomite. The core of
the district near the settlement of Argenta is underlain by Madison Group
1imestones t
Both extrusive and intrusive igneous rocks occur in the district. The
most important of these rocks in terms of the mineralization are quartz
monzonite and granodiorite stocks and andesite porphyry and dacite porphyry
dikes, Shenon (.1931) described the petrography of the various igneous rocks.
The mineralogy of the granitic stocks is andesine, orthoclase, quartz, biotite,
hornblende, and magnetite. The andesite dikes contain andesine phenocrysts in
a finer grained matrix of andesine and augite with accessory magnetite. The
dacite dikes contain phenocrysts of feldspar, quartz, and augite in a very
fine grained felted groundmass.
18
Alluvium"7?
C D
FIGURE 5. --General ized geologic map of the Argenta mining district.
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19
North- to northwest-trending high-angle faults are the predominant
structural features in the district. Major thrust faults are both west and
east of the main part of the district.
Mineralization
Two episodes of mineralization are evident in the district: (1) an early
metasomatic alteration of carbonate rocks that produced a skarn assemblage,
and (2) a later fracture-controlled complex base- and precious-metal metalliza
tion.
The skarn assemblage consists in the most productive areas of garnet,
idocrase, pyroxene, tremolite, calcite, quartz, and epidote. Fine-grained
pyrite and base-metal sulfides occur in the skarn. Large masses of skarn
north of Argenta are composed wholly of fine-grained garnet and quartz. Bleached
recrystallized limestone surrounds the skarn but contains no calc-silicate
minerals.
The complex metal veins occur as tabular shoots along bedding planes and
fissures and as pipe!ike bodies (Shenon, 1931). All of these types occur close
to the contact with the granitic rocks. Alteration adjacent to the veins
consists of quartz and sericite grading outward into a quartz and clay assem
blage. Veins crosscutting the granitic stocks produced intense phyllic
alteration consisting of calcite adjacent to the veins and a weak chloritization
of mafic minerals away from the veins. The dike rocks are intensely altered.
The feldspar is altered to sericite, and the groundmass appears to be mostly
quartz and epidote. The andesite shows a thorough alteration of all feldspar
to sericite, and the mafic minerals are pseudomorphed by chlorite, epidote,
and magnetite,
20
Geochemistry
The geochemical sampling in the district suggests that the predominant
elemental suite is silver, arsenic, cadmium, copper, molybdenum, lead, antimony,
and zinc (table 4). Tin and tungsten are common in all but the western parts
of the district, and bismuth occurs sporadically,
Iron and manganese oxides are the most useful indicators of mineralization.
The calc-silicate hornfels and skarn rocks usually contain silver, lead, and
zinc but do not consistently contain the other trace elements characteristic
of the complex base- and precious-metal mineralization. Likewise, the altered
dike rocks are anomalous in silver, lead, and zinc, but are not anomalous in
the other elements. The altered stocks contain silver, copper, molybdenum,
lead, and zinc; frequently contain tin and tungsten; and infrequently contain
bismuth, Weakly propylitized quartz monzonite west of the Argenta townsite
contains anomalous lead and zinc.
BALDY MOUNTAIN MINING DISTRICT
The Baldy Mountain mining district is in T. 6 S., R. 12 W., 3 miles west
of the Argenta district on the south cide of Baldy Mountain, Gold placers and
lode silver deposits were discovered in the 1860's (Geach, 1972), but production
has been sporadic and there has probably been little actual metal recovered.
After World War II, tungsten was discovered in skarns, but there has been no
economic production.
Geology
The general geology of the district has never been mapped in detail.
Geologic studies are being conducted in conjunction with the current geochemical
studies, and preliminary results indicate that Precambrian, Cambrian, Devonian,
and Mississippian sedimentary rocks are complexly faulted and intruded by the
21
TABLE 4. * Trace elements in ores in the Argenta mining district.
[Parentheses () denote those elements not consistently found in all samples taken from a given deposit.]
Mine/prospect Location Trace-element suite
Unnamed Sec. 30 Ag-As-Bi-Co-Cu-Mo-Pb-Sb-V-W-Zn
Unnamed Sec. 30 Ag-As-Cu-Mo-Pb-Sb-Sn-W-Zn
Iron Mountain West Sec. 30 Ag-As-Cd-Cu-Mo-(Sb)-Pb-Zn
Iron Mountain Sec. 30 Ag-As-Cd-Cu-Pb-Sn-(W)-Zn
Iron Mountain East Sec. 30 Ag-Ba-Cd-Cu-Mo-Pb-Zn
Mauldin Sec. 29 Ag-Pb-Zn
Prospect Sec. 13 Au-Ag-As-Cd-Cu-Mo-Pb-Sb-Sn-W-Zn
Tuscarora Sec. 18 Ag-As-Bi-Cd-Cu-Mo-Pb-Sb-Sn-Zn
Dexter Sec. 17 Ag-Bi-Cd-Cu-Mo-Pb-Sn-(W)-Zn
Mayday Sec. 7 Au-Ag-As-Cd-Cu-Mo-Pb-Sb-V-Zn
Groundhog Sec. 18 Ag-As-Cu-Mo-Pb-Sb-Zn
Midnight South Sec. 24 Ag-As-Cd-Cu-Mo-Pb-Sb-Sn-V-Zn
Argenta Sec. 13 Au-Ag-As-Cd-Cu-Mo-Pb-Sb-Sn-V-Zn
Rena Sec. 18 Ag-As-Cu-Mo-Pb-Zn
Jack Sec. 13 Ag-As-Cd-Cu-Pb-Sb-Zn
Goldfinch Sec. 13 Au-Ag-As-Cu-Pb-Sb-Zn
Dexter East Sec. 16 Ag-As-Cd-Cu-Pb-V-Zn
Yellow Band Sec, 2 Au-Ag-As-B-Mo-Sb-(Zn)
Stinson Sec. 14 Ag-As-Mo-rPb-Sb-Zn
22
Pioneer batholith (D. R. Zimbelman, Aug. 1979, unpublished data)(fig, 6), The
Cambrian formations consist of dolomite, quartzite, and sandy shale. The
Devonian Jefferson Dolomite occurs in the area as thin-bedded carbonaceous
dolomite, Thin- to thick-bedded Madison Group limestones are also present in
the area and are the principal host rocks from the tungsten mineralization.
A gabbro and a granodiorite phase of the Cretaceous Pioneer batholith intrudes
all of the Paleozoic formations and the Precambrian quartzite.
The complexities of the structural setting are not well understood, but
both major thrust faults and high-angle faults are important in the district
(.D. R< Zimbelman, Aug. 1979, unpublished data).
Mineralization
Two episodes of mineralization are evident in the district: (1) an early
skarn alteration of Paleozoic carbonate rocks,, and (2) a fault-controlled
complex base- and precious-metal vein mineralization. Two distinctive types
of skarn were noted during the present study: a dark-green pyroxene-dominant
calc^silicate rock and a garnet-dominant rock.
The pyroxene skarn consists almost wholly of coarse-grained, dark-green
pyroxene with lesser amounts of coarse-grained, zoned, dark-red-brown garnet.
Pyrite is a common accessory mineral. The garnet skarn consists primarily of
red-brown garnet, epidote, pyroxene, calcite, and quartz. Pyrite and chalco-
pyrite are common accessory minerals'.
The vein mineralization consists primarily of quartz with variable amounts
of base-metal sulfides and free milling gold. Most of the ore constituents
observed during this study were oxidized. However, some specimens of pyrite,
galena, chalcopyrite, sphalerite, and tetrahedrite(?) were noted.
23
FIGURE 6.--Preliminary geologic map of the Baldy Mountain mining district (D. R. Zimbelman, Aug. 1979, unpublished data).
I mile
30
,/
Pi I
wc. - j^-
24
Geochemistry
The geochemical sampling in the district suggests that the predominant
element suite in veins is silver, gold, arsenic, bismuth, copper, lead, antimony,
vanadium, and zinc (table 5). Cadmium appears to be present at some localities.
The prefissure vein recrystallization and silication of the rocks makes most
of the host rocks for the complex base-metal-precious-metal veins impermeable
to the later mineralizing solutions. Therefore, away from the fracture systems
the host rocks do not readily give indications of the location of buried veins.
Analyses of iron and manganese oxide coatings on the fractures are the best
indicators of hidden metallization.
The skarns are variable, the pyroxene calc-silicate rock containing
manganese, molybdenum, tin, and tungsten, and the garnet skarn containing some
silver, copper, and zinc in addition to the molybdenum, tin, and tungsten.
DISCUSSION
The similarity of trace-element suites in the several mining districts
suggests the possibility of a common genetic process. The early contact
metasomatism is generally deficient in the base metals and is enriched in
tungsten and molybdenum. These skarns were probably formed at moderately high
temperatures (400°-600°C(?)) and represent a rapid expulsion of the rest of the
aqueous phase from the crystallized pluton now observed at the contact. The
presence of high base-metal content and lower temperature vein deposits
crosscutting the skarn deposits is therefore suggestive of a source somewhat
removed from the observed plutons. Altered feldspar porphyry dikes are present
in all of the mining districts discussed in this report, and these may represent
phases of the later crystallizing magmas that gave rise to the vein occurrences.
25
TABLE 5. Trace elements in ores in the Baldy Mountainmining district.
Mine/prospect Trace-element suite
Nick Preen mines Ag-Bi-Cd-Cu-Pb-Sb
Sec. 24 mine* Ag-As-Cu-Pb-Sb-V-Zn
Old Faithful mine Ag-Au-As-Bi-Cu-Pb-Sb-V-Zn
Sec. 14 Ag-Co-Cu-Zn
Sec, 11 Mn-Mo-Sn-W
Tungsten mill Ag-Bi-Cu-Mo-Sn-V-W
Garret Hill Mn-Mo-Sn-W
Sec. 23 Ag-As-Bi-Mo-Pb-Sb
*Cable mine (?), Geach (1972).
26
In the Bannack and Blue Wing mining districts the geochemical evidence
indicates that the two mining districts may be related to a large hydrothermal
system whose focus is northeast of the Argenta districts (Berger and others,
unpublished data; Siems and others, 1979). If this model is valid, then the
distribution of selected trace elements as well as the styles of mineralization
may point to the center of hydrothermal activity. In the Bannack and Blue Wing
areas this model is illustrated with respect to trace elements by the distribu
tion of tin and barium in the various deposits (table 2), and the style of
mineralization is one of predominantly replacement-type ores on the periphery
of the district (e.g. New Departure mine).
The Argenta mining district is similar to the Bannack area in that mines
in the core of the district contain trace amounts of tin and also tungsten,
and the peripheral mines (e.g., along French Creek and in Ermont) have large
masses of siliceous replacement ores. These features suggest a relationship
to a zoning pattern around an unexposed hydrothermal source. Additional
geochemical work is currently underway to further elucidate any zoning patterns
and to investigate any possible genetic relationships of the Argenta and
Ermont districts,
A ramification for the whole Oil Ion region of the geochemical patterns
and the interrelationships of contact metasomatic deposits and later crosscutting
fissure-vein deposits is that anomalous concentrations of metals may not be
wholly explainable by the geometries of observable rock units. Not all mining
districts are parts of larger systems; however, geochemical indicators similar
to those in the Bannack area that may be found throughout the region should at
least be investigated for the possibility of larger, complex mineralization
systems,
27
RESULTS OF CHEMICAL ANALYSES
The results from the chemical analyses are given in Table 6. All values
are in parts per million except where noted otherwise. The following abbrevi
ations are used in the table:
G, greater than value shown;
N, below level of detection (value given);
L, detected below level of determination (value given);
S, emission spectrographic analysis;
AA, atomic-absorption analysis;
CM, colorimetric analysis;
P, partial extraction.
Sample locations are given in Table 7.
28
TABL
E 6.--Analytical data fr
om rock samples
collected
in mining di
stri
cts
in the
sout
hern
Pi
onee
r Mo
unta
ins,
Be
aver
head
County,
Montana.
onion
OATE
5/ 3/79
NO 1 2 3 4 5 6 7 P 910
1 1
12 13 14 1 5
16 1 7
1 P
19 20 21 22 23 24 25 26
27 2P 29 33'
31 32 33 34 35 36 37 3P 39 40
41 4?43
4445
46 47
4«49 50
SAWPLF
«<M2001
PGI 20
02PG
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PGI 70
04PGI 200 5
PGT 2006
PGI ?007
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200?
PG12009
PGI 2010
PGI 201
1«G
! 20
1 2
P G
I 2 o -n
P G
' 2 0
1 4
P G
[ ? n
1 5
P G
I 2 0
1 6
8GI201 7
PG I 20
1 P
PGT ?ni 9
P G
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» G
T 2 0 2
1PG
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PG I
2024
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? 9
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PF I
203?
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20*iS
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2037
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4 3
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4 4
PF J2045
P F J ? 0
4 6
PF J 2047
«F J ?04P
RFJ ?049
RF J2050
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TABL
E 7.--Longitude
and
latitude for
samp
les
collected
in m
inin
g districts
in the
sout
hern
Pi
onee
r Mo
unta
ins,
Be
aver
head
County,
Montana.
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Table
7.--
Longitude
and
latitude fo
r sample
s collected
in m
inin
g di
stri
cts
in th
e so
uthe
rn Pi
onee
r Mountains, Beaverhead C
ount
y,
Montana,
(continued)
Sample
No
. Latitude Longitude
451<
S?
5 1125209
8M
200
45
16
33
112521?
8
M2
41
1
45
16
33
1125212
REFERENCES
Almond, Hy, 1953, Field method for determination of traces of arsenic in soils:
Analytical Chemistry, v. 25, p. 1766-1767.
Geach, R. D., 1972, Mines and mineral deposits, Beaverhead County, Montana:
Montana Bureau of Mines and Geology Bulletin 85, 194 p.
Grimes, D. J., and Marranzino, A. P., 1968, Direct-current arc and alternating-
current spark emission spectrographic field methods for the semiquantitative
analysis of geologic materials: U.S. Geological Survey Circular 591, 6 p.
Kelly, J. L., 1941, The geology and ore deposits of the Ermont mines: Montana
College of Mineral Science and Technology, B.S. thesis.
Lowell, W. R., 1965, Geologic map of the Bannack-Grayling area, Beaverhead
County, Montana: U.S. Geological Survey Miscellaneous Geologic Investi
gations Map 1-433.
Lyden, C. J., 1948, The gold placers of Montana: Montana Bureau of Mines and
Geology Memoir 26, 152 p.
Myers, W. B., 1952, Geology and mineral deposits of the NW% Will is quadrangle
and adjacent Browns Lake area, Beaverhead County, Montana: U.S. Geological
Survey Open-file Report, 46 p.
Quin, B. F., and Brooks, R. R., 1972, The rapid determination of tungsten in
soils, stream sediments, rocks, and vegetation: Analytica Chimica Acta,
v. 58, p, 301-309.
Shenon, P. J., 1931, Geology and ore deposits of Bannack and Argenta, Beaverhead
County, Montana: Montana Bureau of Mines and Geology Bulletin 6, 80 p.
Siems, D. F., Berger, B. R., and Welsch, E. P., 1979, A comparison of sample
media in developing a geochemical exploration model for stockwork molybdenum
occurrences, Dillon 1° x 2° quadrangle, Montana-Idaho [abs.]: Geological
Society of America, Rocky Mountain Section, Abstracts with Programs, p. 302.
44
U.S. Geological Survey, 1975, Aeromagnetic map of southwestern Montana and
east-central Idaho: U.S. Geological Survey Open-file Report 75-655,
1 sheet.
Ward, F. N., Nakagawa, H. M., Harms, T. F., and VanSickle, G. H., 1969,
Atomic-absorption methods of analysis useful in geochemical exploration:
U.S. Geological Survey Bulletin 1289, p. 20-22.
Welsch, E. P., and Chao, T. T., 1975, Determination of trace amounts of antimony
in geological materials by atomic absorption spectrometry: Analytica
Chimica Acta, v. 76, p. 65-69.
1976, Determination of trace amounts of tin in geological materials by
atomic absorption spectrometry: Analytica Chimica Acta, v. 82, p. 337-342.
Winchell, A. N., 1914, Mining districts of the Dillon quadrangle, Montana, and
adjacent areas; U.S. Geological Survey Bulletin 574, 191 p.
45