rubi copper project, chile - mirasol resources ltd€¦ · 01.11.2017 · rubi project – geology...
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Mirasol Resources Ltd.910-850 West Hastings StreetVancouver, BCCanada V6C 1E1(604) 602-9989www.mirasolresources.comTSXV - MRZ
Mirasol Resources Ltd.910-850 West Hastings StreetVancouver, BCCanada V6C 1E1(604) 602-9989www.mirasolresources.comTSXV - MRZ
Mirasol ResourcesRubi Copper Project, Chile
MIRASOL RESOURCES
Cautionary Statement
This presentation contains certain statements that may be deemed “forward-looking statements”. All statements in this presentation, other than statements of historical fact, thataddress future operations, resource potential, exploration drilling, exploitation activities and events or developments that the Company expects to occur, are forward lookingstatements. Forward looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects”, “plans” “anticipates”,“believes”, “intends”, “estimates”, “projects”, “potential” and similar expressions, or that events or conditions “will”, “would”, “may”, “could” or “should” occur. Informationinferred from the interpretation of drilling results and information concerning mineral resource estimates may also be deemed to be forward looking statements, as it constitutesa prediction of what might be found to be present when and if a project is actually developed. Although the Company believes the expectations expressed in such forward-lookingstatements are based on reasonable assumptions, such statements are not guarantees of future performance and actual results may differ materially from those in the forward-looking statements. Factors that could cause the actual results to differ materially from those in forward-looking statements include market prices, exploitation and explorationsuccesses, and continued availability of capital and financing, and general economic, market or business conditions. Investors are cautioned that any such statements are notguarantees of future performance and actual results or developments may differ materially from those projected in the forward-looking statements. Forward looking statementsare based on the beliefs, estimates and opinions of the Company’s management on the date the statements are made. The Company undertakes no obligation to update theseforward-looking statements in the event that management’s beliefs, estimates or opinions, or other factors, should change, except as may be required by applicable law.
This presentation may use the term “indicated resource”. The Company advises investors that although this term is recognized and required by Canadian securities regulations(under National Instrument 43-101 “Standards of Disclosure for Mineral Projects”), however the US Securities and Exchange Commission does not recognize this term. Investorsare cautioned not to assume that any part of or all of the mineral deposits in these categories will ever be converted into reserves.
Stephen Nano, a “Qualified Person” under National Instrument 43-101, has reviewed and approved the scientific and technical information in this presentation.
RUBI Project – Eocene-Oligocene Porphyry Copper Belt
3
Taltal
Nord
Nix
El Salvador Cluster30 MT Cu
EscondidaCluster
ChuquicamataCluster
Centinela Cluster
Taca Taca
100km
Argentina
Chile
Antofagasta
Santiago
TaltalCopiapo
Base imagery: SRTM DEM
Rubi
Odin
Oligocene AgeMagmatic CentresMirasol Copper Project Copper Deposit/Target
Gold Deposit/TargetMirasol Rubi ProjectLegend
• Large consolidated claim package 25,980 ha - 100% Mirasol owned
• Lithocap – 3.5 km x 2 km area centered on advanced argillic lithocap and < 80 m thick gravel covered extensions zonation vectors to potential porphyry center indicated by low level Cu-Mo mineralization in advanced argillic-phyllic-localized potassic alteration defined from peripheral historic drilling
• Zafiro – 2.8 km x 2.2 km area comprising a gravel covered central magnetic high and depletion halo and peripheral outcropping argillic-phyllic alteration with multiple zones of Cu-Mo anomalous magnetite matrix crackle breccias and stockwork veining Indications of possible exotic copper occurrences
• Portezuelo – 4.5 km x 2.7 km area with coincident zones of magnetite depletion and multiple, outcropping zones of stockworkveining and anomalous Cu-Mo-Au soil and rock chip geochemistry extensive gravel cover
Eocene (34-56 Ma)Paleocene (56-66 Ma)
Diego de Almargo
Base Imagery: ALOS DEM10 km
Radiometric Age Dates
Inca de Oro66 ma
1.6 MT Cu1.7 Moz Au
El SalvadorPCD Cluster
42 ma 17 MT Cu
12 Moz Au
RubiProject49.1-65ma Potrerillos PCD
34.9 ma9 MT Cu
23 Moz Au
Zafiro
PortezueloLithocap
RUBI Project – Location and Infrastructure
4
25 km
El Salvador
Inca De Oro
Carmen
Manto Verde
Potrerillos
Artemisa
MirasolRubi
Project
Chanaral
El SaladoDiego de Almagro
5
C13
C17
C18
PacificOcean • Rubi copper porphyry project located in
Region III of Chile, 80 km east of the port town of Chanaral
• Year round access to main prospects at altitudes between 1,800-2,900 m
• Central portion of project area situated 1 hr drive from Diego de Almagro via well maintained gravel road
• Project situated in prolific Potrerillos District, 15 km south of the El Salvador, and 8 km west of the Potrerillos porphyry Cu deposits and smelter facility
• No protected aquifers or surface water resources
• Good potential synergies with existing nearby infrastructure and nearby, ageing mining operations townships with skilled mining workforce, roads, rail, water, power, smelter
Portrerillos Smelter
Santiago
Taltal
Copiapo
LegendCopper Deposit/Occurrence
Gold-Silver Occurrence
Rubi Project
Powerline
5
1620 1661 1702 1743 1784 1825 1866 1907
Mantos Blancos drilled 36(identified to date) shallow(<150m) holes peripheral totLithocap Prospect in 1980's logging of remnant chips suggest30 holes did not intersectbedrock
2007
Mirasol conducted independentenvironmental, archaeological andsocio-cultural site studies, stream, rockchip and ASD sampling, detailedgeological mapping 3 main targetsgenerated including Lithocap, CornerZone and Portezuelo
10 RC drill holes drilled at PortezueloProspect by unknown company (datingto 1980-90´s) remnant RC chipsvisible but no historic logs or drill assayshave been recovered
FQM - MRZ JV
First Quantum Minerals (FQM) work completed:• Independent environmental, archaeological & socio-cultural site studies; permitting for early stage drilling
approval received for drilling via ´carta de pertenencia´• Geological mapping (1:5000 scale)• Rock chip sampling (142 samples)• ASD/PIMA analysis (SWIR) (1,534 samples)• Soil sampling (787 samples)• Geophysical surveys (~22,870 ha of Airborne Magnetics & Radiometrics, ~8,500 ha of Gravimetry and 36.9 line km
of IP/MT)• Enzyme Leach sampling throughout post mineral gravel covered areas (467 samples)• Buffering Capacity (IDH) sampling throughout post mineral gravel covered areas (467 samples)• Drilling - 16 holes (11 DDH/RC and 5 RC) totaling 6,054.2 m between October 2014 and January 2015 Drilling
focused throughout 6 defined target areas generated from the above work including Glenlivet, Wild Turkey (1stOrder Targets) & Black Label, Jim Beam, Glenfiddich & Jack Daniels (2nd order targets)
2012 September 2013
April 2015
RUBI Project – Work History
• Consolidation and expansion of Rubi claim block from 13,400 ha to 25,980 ha hectares secured tenure peripheral to existing and over newly defined targets
• Remote spectral geology and field mapping Integrated interpretation of alteration, structure and mineralization by an external consultant
• Detailed mapping, rock and stream sampling of Lithocap, Portezuelo, Zafiro. Several additional alteration zones and geophysical targets to be drill-tested
• Re-logging of core from drilling peripheral to the Lithocap Target and alteration/mineralization vector modelling
• Compilation and integrated analysis of Mirasol and FQM data definition of extensive, technically compelling targets that remain untested by drilling and geophysics
Present
Mirasol
US$ 2.8 million – 6,054m drilled
Rubi ProjectTarget Summaries
6
RUBI Project – Geology and Prospective Target Locations
7
5,000m
58.7Ma
65Ma
60Ma
59Ma66Ma
60Ma
61.5Ma62Ma
66.5Ma
60.5Ma
59Ma
50Ma
50Ma
49.1Ma
49.7Ma
Gravel Cover
Gravel Cover
LithocapProspect
PortezueloProspect
UntestedAlterationAnomaly
UntestedAlterationAnomaly
UntestedAlterationAnomaly
Zafiro Prospect• Rubi lies within the Eocene-Oligocene Porphyry Copper
Belt of Northern Chile
• Highly prospective structural setting-setting for Eocene-Oligocene porphyry deposits centred within DomeykoFault Corridor at intersection with trans-origin NW trending Ojos del Salado and NE trending Inca de Oro structural corridors
• Late Cretaceous (~60Ma) andesitic volcanic breccias, flows and porphyritic rocks host the alteration and mineralization
• Paleocene-Eocene granodioritic and pyroxene monzodiorite stocks have intruded the Cretaceous volcanic package
• Age dates on granodioritic to dacitic bodies at the Portezuelo Prospect are dated at 49-50Ma (K/Ar).
Intrusions of this age broadly correlate with the early quartz rhyolite, sanidine phase at the Cerro Pelado Ore body in the El Salvador Porphyry Cluster north of Rubi
• Age dates at Lithocap and Zafiro prospects are currently pending on recently identified mineralization/alteration
• >50% of the Rubi claims are covered by late Tertiary gravel cover observed to locally reach a maximum thickness of 270 m but is generally between 20 and 85 m
• Three untested alteration anomalies have been recently identified; require further follow up
BASE IMAGE: ESRI World Imagery
Rubi Property Boundary
RUBI Project – Lithocap Porphyry Copper Target Summary
Interpreted 3.5 km x 2 km porphyry target below and west of lithocap indicated by:
• 2.3 x 1.7 km outcropping porphyry lithocap, extending under cover. Advanced argillic alteration assemblage (silica, alunite, dickite, kaolinite, jarosite). Structurally controlled along northern boundary that juxtaposes lithocap alteration against patchy intermediate argillic and propylitic assemblages
• Exposed lithocap alteration displays a subtle zonation of high temperature minerals (K/Na alunite, kaolinite/dickite and pyrophyllite) that vectors to the south towards a possible intrusive source
• Drill hole alteration logging suggests transition to higher temperature pyrophyllite + sericite and sericite + chlorite assemblages under lithocap towards the west and south
• Intensity and proportion of potassic/sericitic alteration and brecciation in drill holes increases to north-northwest under the outcropping untested Lithocap
• Sporadic anomalous surface geochemistry highlighted by 4 samples > 40 ppm Mo from leached stockwork zones and strongly anomalous Cu and Mo reported from quartz-tourmaline hydrothermal breccia to the east of the lithocap up to 0.75% and 82 ppm respectively
• 2014 drilling results indicate a vector of anomalous Cu/Mo mineralization towards north/northwest underneath the lithocap outcrop Intersections of 2 m @ 0.16% Cu and 6 m @ 63 ppm Mo
• PDP-IP highlights a strong resistive signature from 100 m depth, coincident with advanced argillic lithocap
• Two strongly anomalous chargeable features are observed between 200-400 m, coincident with lithocap style adv. argillic alteration (dickite-alunite-kaolinite)
• Magnetic anomalies, with signatures interpreted to represent small intrusive bodies occur to the west of the outcropping lithocap
Interpreted 3.5 km x 2 km porphyry Cu target below and west of the outcropping lithocap alteration remains untested by electrical geophysics and drilling interpreted gravel cover depth < 80 m
8
RD-3
RD-102m @ 51.8ppm Mo
RD-132m @ 0.16% Cu
DD-2B2m @ 0.029% Cu
RD-14
RC-7
RD-164m @ 0.1% Cu
RD-154m @ 0.2% Cu
DD-16m @ 63ppm Mo
Magnetic Anomalies
OutcroppingLithocap
1000m
Limit of Interpretation Polylithic Cu BrecciaAssays up to 0.75%
Cu + 82ppm Mo
Chargeability Anomalies (200-400m Depth Slice)
3.5 x 2 kmLithocap Target
Quebrada SaladoAu Vein System
Rubi Property Boundary
Edge of Cover
Gravel Cover
BASE IMAGE: PDP-IP Chargeability on ESRI World Imagery
15
Char
geab
ility
(mV/
V)
0
Gravel Cover
Gravel Cover
Gravel Cover
Cu > 0.05%Mo > 40ppm
MRZ 2014 Drill hole
Rock Chip Geochemistry
Drilling
Historic Drill hole(Penetrated Gravel)
Historic Drill hole(Did not Penetrate Cover)
Alunite + Dickite + KaolinitePyrophyllite + Sericite
Illite + Smectite + Chlorite
Chlorite + Illite
Epidote + Chlorite + Illite
Propylitic
Smectite + Illite
Interpreted Alteration
Polylithic BrecciaVolcanic Breccia
Field Mapping
High temperature potassic/sericitealteration vector
Mapped Stockworking
474.7
425
400
375
350
325
300
275
250
225
200
175
150
125
100
75
50
25
0
RUBI Project – Lithocap Prospect RD-10 Drill Hole Summary
450
474.7
425
400
375
350
325
300
275
250
225
200
175
150
125
100
75
50
25
0
450
Lithocap
Chlorite-illite
Weak Potassic
Andesitic lava with moderate quartz-illite-pyrite alteration.Stockwork with quartz-pyrite
veinlets
Late? Porphyry intrusion with weak potassic alteration
MuscoviteParagonite
Andesitic lava with moderate chlorite-illite-
magnetite alteration.Late anhydrite veinlets
Polymictic explosionbreccia with angular clastswith early? strong potassicalteration with biotite-k-
feldspar.
Lith Alt1
VN 1Alt2
VN 2 VN2Int
Cu % Moppm
Pbppm
Znppm
Auppm
Agppm
0 0.05 0 40 0 100 0 250 0 0.05 0 5
VN1Int
RUBI Project – Zafiro Porphyry Copper Target Summary
10
• Concealed Cu-Mo-Au porphyry target defined by a central magnetic high with peripheral strongly anomalous Cu-Mo stockwork veining and magnetite matrix breccias
• Stream sediment samples taken from drainages incising the valley scarp are strongly anomalous in Cu with 6 samples > 0.05% Cu possible evidence of a buried porphyry source or exotic copper mineralization within prospect
• Mineralized andesitic porphyry and crackle breccia outcrops exposed along NW oriented valley scarp on NE edge of property and target boundary, recorded assays up to 3.09g/t Au, 0.08% Cu and 110.5ppm Mo
• 3D Magnetic inversion, 750 m depth slice indicate a 2.8 x 2.2 km magnetic high, interpreted to be a concealed intrusive complex under gravel cover SW gravel plateau hosting target area interpreted to be < 160 m thick
• Magnetic high surrounded by strong magnetic depletion zone interpreted as a phyllicalteration halo, as observed in holes DD-2B (2m @290 ppm Cu) and RC-9 (4m @ 59.4 ppm Mo)
• Cu-Mo-Au mineralization outcropping in valley scarp below cover is associated with magnetite matrix crackle breccias and qtz-limonite stockwork veining hosted in andesitic porphyry volcanics. Strongly anomalous Cu, Mo and Pb assays associated, up to 0.28%, 3220ppm and 10250ppm respectively
• Limited pIR-SPEC sampling along outcrop on the valley slope in the NW, confirms presence of high temperature phyllic alteration (Na-K rich paragonite and muscovite) coincident with anomalous geochemistry
• Remnant outcrop of adv. argillic (dickite-alunite-kaolinite) lithocap style alteration in the north and northwest with propylitic (chlorite-epidote- magnetite) pervasive alteration and hydrothermal veining
Vectors of alteration and mineralization indicate potential for the magnetic high to be related to a copper bearing porphyry intrusive that remains untested by electrical geophysics and drilling
RD-3
RD-102m @ 51.8ppm Mo
RD-132m @ 0.36% Cu& 22.2ppm Mo
RC-94m @ 59.4ppm Mo
Magnetic Depletion(Interpreted Phyllic Alteration Halo)
Magnetic High(Concealed Intrusive?)
Mineralised Crackle Breccias exposed in valley scarp.
Anomalous Cu-Mo-Au-As
DD-2B2m @ 0.029% Cu
Mineralized Andesitic Porphyry exposed in
valley scarp
Remnant Adv.Argillic
Lithocap
BASE IMAGE:3D Magnetic Inversion
750m Depth SliceOn ESRI World Imagery
1000m
Rubi Property Boundary
2.8 x 2.2 kmZafiro Target
Strongly anomalous Cu-Mo-Pb±Au-Ag geochem associated
with qtz-hem-magnetite stockworking
6 strongly anomalous stream sediment samples assayed >0.05% Cu
from drainages along valley scarp
Cu > 0.05%Mo > 40ppm
MRZ 2014 Drill hole
Rock Chip GeochemistryDrilling
Historic Drill hole(Penetrated Gravel)
Mapped Stockworking
Historic Drill hole(Did not penetrate cover)
Polylithic Breccia
Andesitic Porphyry
Field Mapping
Volcanic Breccia
Crackle Breccia
Stream GeochemistryCu > 0.05%
Cu oxide mineralization in
gravels
RUBI Project – Zafiro Prospect Summary
• Majority of prospect covered by gravels interpreted to average less than 150m thick. Localised indications of possible exotic Cu in shallow workings hosted in gravel Cu source unclear
• North and NE of the core of the target mineralization is hosted by phyllicor propyltic altered Cretaceous volcanic sequence comprising andesitic lava and pyroclastic rock
• Monomictic hydrothermal breccia with andesitic clasts cemented by hematite matrix (after magnetite) and argillic alteration developed in NE outcropping portion of Cretaceous volcanic sequence indicating proximity to intrusive center
• Local development to NW of target of thin and discontinuous quartz and siderite veinlet stockworks with sulphide clots and green oxide Cu hosted in fine grained, strongly chlorite-magnetite-illite altered rock indicate peripheral porphyry mineralization
Primary target comprises a large covered magnetic anomaly with a strong magnetic depletion halo with peripheral outcropping alteration and mineralization consistent with the outer zones of a porphyry copper system
11
MCR0019346. Massive quartz vein withsulphide clots and green Cu oxide.
432ppm As, 0.285% Cu, 3,220ppm Mo, 10,250ppm Pb, 20.3ppm Sb, 292ppm Zn
Zafiro stockwork zone quartz-carbonate veinlets up to 0.05% Cu
MCR0019280. Hydrothermally brecciatedandesitic lava with hematite brecciamatrix (after magnetite) 133ppm Cu,
13.95ppm Mo
Cobbles of high Cu grade, exotic Cu oxides, from historic workings hosted in gravel
cover
Hydrothermal breccia body hosting argillic+ feox alteration
MCR0019353. Massive quartz vein fromstockwork zone. 73ppm As, 77ppm Cu, 41.5ppm Mo, 337ppm Pb, 119ppm Zn
1. 2. 3.
4. 5. 6.
1.2.
3.4.
5.
6.
1,000m
ZafiroTarget
RUBI Project – Portezuelo Porphyry Copper Target Summary
• Large 4.5km x 2.7km dominantly concealed to shallowly covered Cu-Mo-Au porphyry target defined by: • Strongly anomalous Cu-Mo geochemistry (up to 0.96% Cu,
3,500ppm Mo) associated with qtz-limonite stockwork zones within a larger Cu-Mo soil geochemical anomaly Cu up to 0.21%, Mo up to 100ppm
• Elongate 1,200 x 600 m covered magnetic anomaly with coincident Cu-Mo±As-Au-Ag rock chip geochemistry
• Historic drilling (results not available) tested only a minor portion of the outcropping system at shallow depths
• Widespread gravel cover, with sporadic outcrop of granodiorite intrusive and quartz-limonite stockwork veining in biotite hornfels
• 49-50ma granodioritic to dacitic intrusive phase broadly correlative with pre-mineral intrusive phases at El Salvador
• Outer, distal, sub epithermal, polymetallic (Cu-Mo+Pb-Zn-Sb ± Ag-Au) veining, structurally hosted mineralisation
• Cu-Mo-Au mineralisation associated with qtz-limonite stockwork veining
• An arcuate, low temperature phengitic halo bounds the east of the target based on pIRSPEC White Mica temperature & composition analysis
• Other extensive outcropping and covered target zones warrant followup mapping and geochemical sampling and remain untested by electrical geophysics and drilling
12
Gravel Cover
Cu > 0.05% Rock chipMo > 40ppm Rock chip
Higher TemperatureWhite Mica
Geochem
pIR-SPEC Sampling
Lower TemperatureWhite Mica
Observed Stockworkingand/or veiningHistoric Drill hole
Cu Soil AnomalyMo Soil Anomaly
Rubi Property Boundary
Covered Magnetic Anomaly(concealed intrusive?)
BASE IMAGE: RTP Heli-Magnetics500m
4.5 x 2.7 km Portezuelo Target
Rubi Property Boundary
Strongly anomalous rock chip assays, Au to 11g/t, 5 samples > 1g/t Au. Pb to 19,650ppm, Zn to 5,180 and Sb to 79.5ppm
Limit of anomalous Cu/Mo in previous JV partner soil sampling, ground followup required
Qtz-Hematite ± Goethite-Limonite Stockwork/Sheeted vein outcrops (assays up to 0.21% Cu, 209ppm Mo and 1.68g/t Au)
• Well developed sheeted and/or stockwork limonite-sericite-silica veining and fracture controlled sericitisation broadly coincident with zone of magnetite depletion in magnetic survey
• Strong Cu-Mo signature reporting to quartz-Fe oxide ± Cu ox stockwork hosted by granodiorite/tonalite intrusive rocks
• Hematite-goethite-quartz breccia and veining developed in biotite hornfels in sporadic outcrop in north east of Portezuelo area Favourable host for porphyry vein development
• Historic (1980’s) drilling has only tested a small portion of the outcropping system
• No systematic mapping and sampling, geophysics or drilling carried out subsequent to historic 1980’s drilling
• Several additional defined targets merit further mapping and geochemical sampling 13
Hematite-goethite breccia developed on biotite hornfels throughout NE portion of Portezuelo
Limonite-goethite and quartz-hematite-goethite stockwork at Portezuelo North West
K-spar alteration and qtz stockwork(0.16% Cu, 209ppm Mo, 370ppm Zn)
Stockwork of quartz/limonite in argillic altered granodiorite (657ppm Cu, 0.38g/t Au)
Potassic Altered Diorite with Leached Qtz-Limonite Stockwork (973ppm Cu, 104ppm Mo)
Green copper oxide in granodiorite
Stockworking and late stage dyking in granodiorite (370ppm Cu)
Quartz sheeted veining in granodiorite (0.15% Cu, 844ppm Pb, 644ppm Zn)
RUBI Project – Portezuelo Prospect Summary
Sheeted Qtz-Limonite Veins Potassic phyllicaltered porphyry over 200m in Road cut
(0.12% Cu, 121ppm Mo)
1. 2. 3.
4. 5.
7. 8. 9.
1.2.
3. 4.
5.
6.
7. 8.
9. 500m
6.
RUBI Copper Porphyry Project – Summary
• Located within 25,980 ha 100% Mirasol owned block, in Region III of Chile, 80 km east of port town of Chañaral, key target areas between 1,800-2,900 m altitude
• Positioned in highly prospective regional-scale geological setting for Eocene-Oligocene porphyry deposits centred within Domeyko Fault Corridor at intersection with trans-origin NW trending Ojos del Salado and NE trending Inca de Oro structural corridors
• Located 15 km southwest of El Salvador Porphyry Cu Mine and 10 km west of Potrerillos Porphyry Cu Mine and smelter
• No significant identified environmental, sociocultural nor indigenous community impediments to exploration1
• Existing nearby infrastructure townships with skilled mining workforce, roads, rail, water, power, smelter
3 large, primary porphyry centre target prospects remain untested by electrical geophysics and drilling: Lithocap, Zafiro and Portezuelo
• Lithocap – 3.5 km x 2 km target area centered on advanced argillic lithocap and < 80 m thick gravel covered extensions zonation vectors to potential porphyry center indicated by low level Cu-Mo mineralization in advanced argillic-phyllic-localized potassic alteration defined from peripheral historic drilling
• Zafiro – 2.8 km x 2.2 km target area comprising a gravel covered central magnetic high with depletion halo and peripheral outcropping argillic-phyllic alteration with multiple zones of Cu-Mo geochemically anomalous magnetite matrix crackle breccias and qtz-hematite stockwork veining with indications of possible laterally developed exotic copper occurrences in gravel cover
• Portezuelo – 4.5 km x 2.7 km target area with coincident zones of magnetite depletion and multiple, intermittently outcropping zones of stockwork and sheeted veining and anomalous Cu-Mo-Au soil and rock chip geochemistry throughout extensive zones of shallow gravel cover
Primary target areas require additional work to refine drill hole placement via systematic geology, geochemistry and electrical geophysics
Several additional, recently defined alteration/geochemical targets that require followup exploration
Mirasol seeking a quality partner via earn in JV deal to undertake systematic exploration at the project1Archaeological sensitivity peripheral to Lithocap Target identified and successfully permitted and managed during previous JV partner drill program
14
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