General Information
Secondary Commodities: copper, zinc, lead
Deposit Type(s): Volcanogenic Massive Sulphide (VMS) Kuroko Cu-Pb-Zn
Location(s): 61.408330 N, -130.094440 W
NTS Mapsheet(s): 105G08
Location Comments: .5 Kilometres
Hand Samples Available at YGS: No
Capsule
Work History
Staked as Puck cl 1-89 (YB55979) in Sep/94 by Expatriate Resources Ltd which carried out grid soil sampling, prospecting and preliminary geological mapping the following year. In Nov/95 Westmin Resources Ltd flew an airborne geophysical program over the claims as part of a larger regional survey. In Dec/95 Westmin optioned the claims as part of a larger joint venture agreement with Expatriate.
In 1996 Westmin carried out ground Max-min, mag and VLF geophysical programs over the claims followed by a 4 hole (908.9 m) diamond drill program. In Sep/96 Westmin and Expatriate formalized their option agreement and later in the fall, drilled 2 additional diamond drill holes (425.5 m). In Oct/96 Westmin staked Cup fractional cl 1-24 (YB87695) to cover gaps identified during a claim survey.
During the 1997 field season Westmin completed further ground geophysics and soil sampling and drilled 10 additional diamond drill holes (2 691 m). In Mar/98 Westmin Resources was acquired by Boliden Ltd.
In Apr/99 Expatriate Resources Ltd purchased all of Westmin¿s holdings in the Finlayson Lake district, including Westmin¿s 50% interest in the Puck/Cup claims, from Boliden, resulting in Expatriate reclaiming 100% interest in the claims.
In 2000, Expatriate drilled 1 diamond drill hole (344.12 m) on Foot cl #2 located across the claim boundary from the Puck claims.
Capsule Geology
The area is underlain by a Mississippian to Permian age, mixed volcano-sedimentary package belonging to the Yukon-Tanana Terrane (YTT). The YTT is a volcanic-plutonic, pericratonic arc assemblage that was strongly deformed and metamorphosed by late Triassic time. Volcanic hosted massive sulphide deposits exist at different stratigraphic positions within the YTT including the Fyre Lake deposit (Minfile Occurrence #105G 034) in Devonian to Early Mississippian Fire Lake mafic meta-volcanic unit (DMF), the Kudz Ze Kayah deposit (Minfile Occurrence #105G 117) in the Mississippian Kudz Ze Kayah felsic meta-volcanic unit (MK), the Wolverine deposit within the Carboniferous Wolverine Lake succession, and the Ice deposit (Minfile Occurrence #105G 118) within Pennsylvanian to Permian Campbell Range basalts.
The Puck claims cover the southern extension of the stratigraphic package which hosts the Wolverine deposit (Minfile Occurrence #105G 072), located 2.5 km to the northwest and the Sable zone located 250 m to the northwest. The Wolverine deposit, Sable zone and Puck occurrence are underlain by Murphy and Piercey¿s Carboniferous Wolverine Lake Succession (1999; 2000) consisting predominantly of carbonaceous phyllite and quartz sandstone (unit CWcp) overlain by a thin band of platy brown limestone (unit CWl) and thinly interbedded, massive to granular siliceous rock and phyllite (metatuff and exhalite) and baritic iron formation (unit CWt). On the northeast side of the property the Wolverine Lake Succession is overlain by the Pennsylvanian to Permian Campbell Range Succession comprised primarily of coarse basaltic breccia (unit ]PCb1), carbonaceous argillite, sandstone and grey quartz grit (unit ]PCs), and coarse basaltic breccia (unit ]PCb2).
Murphy and Piercey of the Yukon Geology Program report that the Wolverine massive sulphide deposit and nearby mineralized zones (Fisher, Lynx, Sable) occur near the contact between unit CWcp, carbonaceous phyllite and quartz sandstone and unit CWt, massive to granular siliceous rock and lightly-colored phyllite. The baritic iron formation located near its base is employed as a marker. Bradshaw et al., who have carried out more detailed geological mapping, place the deposit at the contact between their units 5 and 6 which they define slightly different from Murphy and Piercey¿s units. Despite these differences, both groups place the deposit above the carbonaceous phyllite and below the overlying siliceous rocks.
The massive sulphides at the Wolverine deposit are hosted in either argillite or aphyric rhyolite. Carbonaceous argillite and a porphyritic felsic unit form the immediate footwall to the mineralization. Piercey et al. (2001) demonstrate that the Wolverine deposit, Sable zone and Puck occurrence are underlain by subvolcanic porphyritic intrusions located approximately 10-20 m beneath the exhalative sulphide bodies or iron formation. Interlayered carbonaceous argillites, felsic volcanic, fragmental and tuffaceous units and up to three beds of exhalite magnetite carbonate iron formation occur in the hanging wall. The massive tabular sulphide body is zoned, polymetallic, and displays banded, clastic and massive replacement textures. The deposit is located stratigraphically above the Kudz Ze Kayah deposit (Minfile Occurrence #105G 117) located 20 kilometres to the west.
At the Wolverine deposit sulphide intersections commonly have Mg-chlorite footwall alteration zones enveloping pyrite/ chalcopyrite/pyrrhotite stringer mineralization (Tucker et al., 1997). The main sulphide minerals, in order of decreasing abundance, are pyrite, sphalerite, chalcopyrite, and galena. Argentian tetrahedrite contains more than 90% of the silver in the deposit, the remainder occurring in solid solution with galena and in Au-Ag solid solution series. Au is present as Ag-rich native gold and Au-rich native silver. Gangue minerals associated with the massive sulphide are comprised of quartz, muscovite, calcite and dolomite-ankerite. Texturally the sulphide minerals are generally fine to medium grained. Ore minerals occur either interstitial to pyrite or as a matrix for disseminated pyrite (Tucker et al., 1997).
In 1995, the Expatriate conducted a prospecting and grid soil sampling program on the Puck claims. Extensive till coverage on the property resulted in a subdued geochemical response. Copper analysis returned the best results, highlighting a 1 200 by 1 000 m zone of weakly to moderately anomalous values at the north end of the property. Diamond drilling in 1996 and 1997 (4 025m in 16 holes) did not intersect massive sulphides but did confirm the presence of the favourable ¿Wolverine horizon¿, magnetite horizon, stockwork mineralization and strong alteration. Drill intersections included values such as; >10 000 ppm Cu, 1.16% Pb and 2.72% Zn (Turner and Terry, 1998). Westmin reports that the most promising target is located 250 metres east of the property boundary, where hole PK97-16 cut stockwork mineralization thought to be related to massive sulphide mineralization intersected in the neighbouring Sable Zone.
The single drill hole collared on Foot cl #2 was designed to test the down dip extension of high-grade sulphide mineralization found at the Sable zone. The hole failed to intersect economic mineralization.
References
BOND, J.D., MURPHY, D.C., COLPRON, M., GORDEY, S.P., PLOUFFE, A., ROOTS, C.F., LIPOVSKY, P.S., STRONGHILL, G., AND ABBOTT, J.G., 2002. Digital compilation of bedrock geology and till geochemistry, northern Finlayson Lake map area, Southeastern Yukon (105G), Exploration and Geological Services Division, Yukon Region, Indian and Northern Affairs Canada, Open File Report, 2002-7(D) and Geological Survey of Canada Open File 4243.
BRADSHAW, C.D., TUCKER, T.L., PETER, J.M., PARADIS, S., AND ROWINS, S.M., 2001. Geology of the Wolverine polymetallic volcanic-hosted massive sulphide deposit, Finlayson Lake District, Yukon Territory, Canada. In: Yukon Exploration and Geology 2000, D.S. Emond and L.H. Weston (eds.), Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p. 269-287.
EXPATRIATE RESOURCES LTD, Apr/96. Assessment Report #093414 by W.A. Wengzynowski.
EXPATRIATE RESOURCES LTD, Sep/2001. Assessment Report #094239 by R. Duncan et al.
EXPATRIATE RESOURCES LTD, News Release. 9 Sep/96; 21 Jul/97; 4 Nov/97.
EXPATRIATE RESOURCES LTD, Feb/2001. Web Site: www.expatriateresources..com
GEOLOGICAL SURVEY OF CANADA Paper 75-lA, p. 45-48.
HUNT, J.A., 1997. Massive Sulphide deposits in the Yukon-Tanana and adjacent Terranes. In: Yukon Exploration and Geology 1996, Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p. 35-45.
MURPHY, D.C. and PIERCEY, S.J., 1999. Geological map of parts of Finlayson Lake (105G/7, 8 and parts of 1, 2, and 9) and Frances Lake (parts of 105H/5 and 12) map areas, southeastern Yukon (1:100 000-scale). Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, Open File 1999-4.
MURPHY, D.C. AND PIERCEY, S.J., 2000. Syn-mineralization faults and their re-activation, Finlayson Lake massive sulphide district, Yukon-Tanana Terrane, southeastern Yukon. In: Yukon Exploration and Geology 1999, D.S. Emond and L.H. Weston (eds.), Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p. 55-66.
MURPHY, D.C., COLPRON, M., GORDEY, S.P., ROOTS, C.F., ABBOTT, G., AND LIPOVSKY, P.S., 2001. Preliminary bedrock geological map of northern Finlayson Lake area (NTS 105 G) Yukon Territory (1:100 000 scale). Exploration and Geological Services Division, Yukon Region, Indian and Northern Affairs Canada, Open File 2001-33.
MURPHY, D.C., COLPRON, M., ROOTS, C.F., GORDEY, S.P. AND ABBOTT, J.G., 2002. Finlayson Lake Targeted Geoscience Initiative (southeastern Yukon) , Part 1: Bedrock geology. In: Yukon Exploration and Geology 2001, D.S. Emond, L.H. Weston and L.L. Lewis (eds.), Exploration and Geological Services Division, Yukon Region, Indian and Northern Affairs Canada, p. 189-207.
PIERCEY, S.J., PETER, J.M., BRADSHAW, G.D., TUCKER, T. and PARADIS, S., 2001. Geological characteristics of high-level subvolcanic intrusions porphyritic intrusions associated with the Wolverine Zn-Pb-Cu volcanic-hosted massive sulphide deposit, Finlayson Lake District, Yukon, Canada. In: Yukon Exploration and Geology 2000, D.S. Emond and L.H. Weston (eds.), Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p. 335-346.
TUCKER, T.L., et al. 1997. Wolverine Massive Sulfide project, Yukon Territory, Canada-Westmin Resources Ltd and Atna Resources Ltd, Vancouver, B.C. In: Yukon Exploration and Geology 1996, Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p.53-55.
WESTMIN RESOURCES LTD, May/97. Assessment Report #093652 by A.J. Turner and D.A. Terry.
WESTMIN RESOURCES LTD, May/98. Assessment Report #093790 by A.J. Turner and D.A. Terry.
WESTMIN RESOURCES LTD., Nov/95. Wolverine Lake Project.
WESTMIN RESOURCES LTD., 1997. Exploration Review.
WESTMIN RESOURCES LTD., News Release. 18 Jul/96; 17 Oct/96
YUKON EXPLORATION & GEOLOGY 1994, p. 8; 11. 1995, p. 11; 17. 1996, p. 15; 31. 1997; p. 37. 1998; p.37.
YUKON GEOLOGY AND EXPLORATION 1979-80, p. 94-96. 1982, p. 128; 1983, p. 177.
Staked as Puck cl 1-89 (YB55979) in Sep/94 by Expatriate Resources Ltd which carried out grid soil sampling, prospecting and preliminary geological mapping the following year. In Nov/95 Westmin Resources Ltd flew an airborne geophysical program over the claims as part of a larger regional survey. In Dec/95 Westmin optioned the claims as part of a larger joint venture agreement with Expatriate.
In 1996 Westmin carried out ground Max-min, mag and VLF geophysical programs over the claims followed by a 4 hole (908.9 m) diamond drill program. In Sep/96 Westmin and Expatriate formalized their option agreement and later in the fall, drilled 2 additional diamond drill holes (425.5 m). In Oct/96 Westmin staked Cup fractional cl 1-24 (YB87695) to cover gaps identified during a claim survey.
During the 1997 field season Westmin completed further ground geophysics and soil sampling and drilled 10 additional diamond drill holes (2 691 m). In Mar/98 Westmin Resources was acquired by Boliden Ltd.
In Apr/99 Expatriate Resources Ltd purchased all of Westmin¿s holdings in the Finlayson Lake district, including Westmin¿s 50% interest in the Puck/Cup claims, from Boliden, resulting in Expatriate reclaiming 100% interest in the claims.
In 2000, Expatriate drilled 1 diamond drill hole (344.12 m) on Foot cl #2 located across the claim boundary from the Puck claims.
Capsule Geology
The area is underlain by a Mississippian to Permian age, mixed volcano-sedimentary package belonging to the Yukon-Tanana Terrane (YTT). The YTT is a volcanic-plutonic, pericratonic arc assemblage that was strongly deformed and metamorphosed by late Triassic time. Volcanic hosted massive sulphide deposits exist at different stratigraphic positions within the YTT including the Fyre Lake deposit (Minfile Occurrence #105G 034) in Devonian to Early Mississippian Fire Lake mafic meta-volcanic unit (DMF), the Kudz Ze Kayah deposit (Minfile Occurrence #105G 117) in the Mississippian Kudz Ze Kayah felsic meta-volcanic unit (MK), the Wolverine deposit within the Carboniferous Wolverine Lake succession, and the Ice deposit (Minfile Occurrence #105G 118) within Pennsylvanian to Permian Campbell Range basalts.
The Puck claims cover the southern extension of the stratigraphic package which hosts the Wolverine deposit (Minfile Occurrence #105G 072), located 2.5 km to the northwest and the Sable zone located 250 m to the northwest. The Wolverine deposit, Sable zone and Puck occurrence are underlain by Murphy and Piercey¿s Carboniferous Wolverine Lake Succession (1999; 2000) consisting predominantly of carbonaceous phyllite and quartz sandstone (unit CWcp) overlain by a thin band of platy brown limestone (unit CWl) and thinly interbedded, massive to granular siliceous rock and phyllite (metatuff and exhalite) and baritic iron formation (unit CWt). On the northeast side of the property the Wolverine Lake Succession is overlain by the Pennsylvanian to Permian Campbell Range Succession comprised primarily of coarse basaltic breccia (unit ]PCb1), carbonaceous argillite, sandstone and grey quartz grit (unit ]PCs), and coarse basaltic breccia (unit ]PCb2).
Murphy and Piercey of the Yukon Geology Program report that the Wolverine massive sulphide deposit and nearby mineralized zones (Fisher, Lynx, Sable) occur near the contact between unit CWcp, carbonaceous phyllite and quartz sandstone and unit CWt, massive to granular siliceous rock and lightly-colored phyllite. The baritic iron formation located near its base is employed as a marker. Bradshaw et al., who have carried out more detailed geological mapping, place the deposit at the contact between their units 5 and 6 which they define slightly different from Murphy and Piercey¿s units. Despite these differences, both groups place the deposit above the carbonaceous phyllite and below the overlying siliceous rocks.
The massive sulphides at the Wolverine deposit are hosted in either argillite or aphyric rhyolite. Carbonaceous argillite and a porphyritic felsic unit form the immediate footwall to the mineralization. Piercey et al. (2001) demonstrate that the Wolverine deposit, Sable zone and Puck occurrence are underlain by subvolcanic porphyritic intrusions located approximately 10-20 m beneath the exhalative sulphide bodies or iron formation. Interlayered carbonaceous argillites, felsic volcanic, fragmental and tuffaceous units and up to three beds of exhalite magnetite carbonate iron formation occur in the hanging wall. The massive tabular sulphide body is zoned, polymetallic, and displays banded, clastic and massive replacement textures. The deposit is located stratigraphically above the Kudz Ze Kayah deposit (Minfile Occurrence #105G 117) located 20 kilometres to the west.
At the Wolverine deposit sulphide intersections commonly have Mg-chlorite footwall alteration zones enveloping pyrite/ chalcopyrite/pyrrhotite stringer mineralization (Tucker et al., 1997). The main sulphide minerals, in order of decreasing abundance, are pyrite, sphalerite, chalcopyrite, and galena. Argentian tetrahedrite contains more than 90% of the silver in the deposit, the remainder occurring in solid solution with galena and in Au-Ag solid solution series. Au is present as Ag-rich native gold and Au-rich native silver. Gangue minerals associated with the massive sulphide are comprised of quartz, muscovite, calcite and dolomite-ankerite. Texturally the sulphide minerals are generally fine to medium grained. Ore minerals occur either interstitial to pyrite or as a matrix for disseminated pyrite (Tucker et al., 1997).
In 1995, the Expatriate conducted a prospecting and grid soil sampling program on the Puck claims. Extensive till coverage on the property resulted in a subdued geochemical response. Copper analysis returned the best results, highlighting a 1 200 by 1 000 m zone of weakly to moderately anomalous values at the north end of the property. Diamond drilling in 1996 and 1997 (4 025m in 16 holes) did not intersect massive sulphides but did confirm the presence of the favourable ¿Wolverine horizon¿, magnetite horizon, stockwork mineralization and strong alteration. Drill intersections included values such as; >10 000 ppm Cu, 1.16% Pb and 2.72% Zn (Turner and Terry, 1998). Westmin reports that the most promising target is located 250 metres east of the property boundary, where hole PK97-16 cut stockwork mineralization thought to be related to massive sulphide mineralization intersected in the neighbouring Sable Zone.
The single drill hole collared on Foot cl #2 was designed to test the down dip extension of high-grade sulphide mineralization found at the Sable zone. The hole failed to intersect economic mineralization.
References
BOND, J.D., MURPHY, D.C., COLPRON, M., GORDEY, S.P., PLOUFFE, A., ROOTS, C.F., LIPOVSKY, P.S., STRONGHILL, G., AND ABBOTT, J.G., 2002. Digital compilation of bedrock geology and till geochemistry, northern Finlayson Lake map area, Southeastern Yukon (105G), Exploration and Geological Services Division, Yukon Region, Indian and Northern Affairs Canada, Open File Report, 2002-7(D) and Geological Survey of Canada Open File 4243.
BRADSHAW, C.D., TUCKER, T.L., PETER, J.M., PARADIS, S., AND ROWINS, S.M., 2001. Geology of the Wolverine polymetallic volcanic-hosted massive sulphide deposit, Finlayson Lake District, Yukon Territory, Canada. In: Yukon Exploration and Geology 2000, D.S. Emond and L.H. Weston (eds.), Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p. 269-287.
EXPATRIATE RESOURCES LTD, Apr/96. Assessment Report #093414 by W.A. Wengzynowski.
EXPATRIATE RESOURCES LTD, Sep/2001. Assessment Report #094239 by R. Duncan et al.
EXPATRIATE RESOURCES LTD, News Release. 9 Sep/96; 21 Jul/97; 4 Nov/97.
EXPATRIATE RESOURCES LTD, Feb/2001. Web Site: www.expatriateresources..com
GEOLOGICAL SURVEY OF CANADA Paper 75-lA, p. 45-48.
HUNT, J.A., 1997. Massive Sulphide deposits in the Yukon-Tanana and adjacent Terranes. In: Yukon Exploration and Geology 1996, Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p. 35-45.
MURPHY, D.C. and PIERCEY, S.J., 1999. Geological map of parts of Finlayson Lake (105G/7, 8 and parts of 1, 2, and 9) and Frances Lake (parts of 105H/5 and 12) map areas, southeastern Yukon (1:100 000-scale). Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, Open File 1999-4.
MURPHY, D.C. AND PIERCEY, S.J., 2000. Syn-mineralization faults and their re-activation, Finlayson Lake massive sulphide district, Yukon-Tanana Terrane, southeastern Yukon. In: Yukon Exploration and Geology 1999, D.S. Emond and L.H. Weston (eds.), Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p. 55-66.
MURPHY, D.C., COLPRON, M., GORDEY, S.P., ROOTS, C.F., ABBOTT, G., AND LIPOVSKY, P.S., 2001. Preliminary bedrock geological map of northern Finlayson Lake area (NTS 105 G) Yukon Territory (1:100 000 scale). Exploration and Geological Services Division, Yukon Region, Indian and Northern Affairs Canada, Open File 2001-33.
MURPHY, D.C., COLPRON, M., ROOTS, C.F., GORDEY, S.P. AND ABBOTT, J.G., 2002. Finlayson Lake Targeted Geoscience Initiative (southeastern Yukon) , Part 1: Bedrock geology. In: Yukon Exploration and Geology 2001, D.S. Emond, L.H. Weston and L.L. Lewis (eds.), Exploration and Geological Services Division, Yukon Region, Indian and Northern Affairs Canada, p. 189-207.
PIERCEY, S.J., PETER, J.M., BRADSHAW, G.D., TUCKER, T. and PARADIS, S., 2001. Geological characteristics of high-level subvolcanic intrusions porphyritic intrusions associated with the Wolverine Zn-Pb-Cu volcanic-hosted massive sulphide deposit, Finlayson Lake District, Yukon, Canada. In: Yukon Exploration and Geology 2000, D.S. Emond and L.H. Weston (eds.), Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p. 335-346.
TUCKER, T.L., et al. 1997. Wolverine Massive Sulfide project, Yukon Territory, Canada-Westmin Resources Ltd and Atna Resources Ltd, Vancouver, B.C. In: Yukon Exploration and Geology 1996, Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p.53-55.
WESTMIN RESOURCES LTD, May/97. Assessment Report #093652 by A.J. Turner and D.A. Terry.
WESTMIN RESOURCES LTD, May/98. Assessment Report #093790 by A.J. Turner and D.A. Terry.
WESTMIN RESOURCES LTD., Nov/95. Wolverine Lake Project.
WESTMIN RESOURCES LTD., 1997. Exploration Review.
WESTMIN RESOURCES LTD., News Release. 18 Jul/96; 17 Oct/96
YUKON EXPLORATION & GEOLOGY 1994, p. 8; 11. 1995, p. 11; 17. 1996, p. 15; 31. 1997; p. 37. 1998; p.37.
YUKON GEOLOGY AND EXPLORATION 1979-80, p. 94-96. 1982, p. 128; 1983, p. 177.
Location Map
Last Updated: Sep 13, 2018
Work History
| Year | Work Type | Comment |
|---|---|---|
| 2000 | Drilling: Diamond | One hole, 344 m. Expatriate drilled I drill hole on Foot claim #2 located across claim boundary from Puck claims. |
| 1997 | Drilling: Diamond | Ten holes, 2,691 m. |
| 1997 | Geochemistry: Soil | |
| 1997 | Ground Geophysics: Magnetics | Also Max-Min survey. |
| 1996 | Airborne Geophysics: Electromagnetic | Also magnetic survey. |
| 1996 | Drilling: Diamond | Four holes, 908.9 m, followed by two holes, 425.5 m later in year. |
| 1996 | Ground Geophysics: Magnetics | Also Max-Min and VLF surveys. |
| 1995 | Other: Prospecting | |
| 1995 | Geochemistry: Soil | |
| 1995 | Geology: Bedrock Mapping |
Regional Geology - Terrane
Group: Intermontane
Affinity: W Laurentia
Name: Yukon-Tanana
Realm: peri-Laurentian
Regional Geology - Bedrock
Supergroup:
Group/Suite: Wolverine Lake
Formation:
Member:
Terrane: Yukon-Tanana
Period Max: Carboniferous
Age Max: 357 MA
Period Min: Carboniferous
Age Min: 345 MA
Rock Major: carbonaceous phyllite
Rock Minor: sandstone
Reference: Murphy et al. (2001) - YGS OF 2001-33
Geological Unit (1M): DMF
Geological Unit (250K): DMF3
Assessment Reports that overlap occurrence
| Report Number | Year | Title | Worktypes | Holes Drilled | Meters Drilled |
|---|---|---|---|---|---|
| 097243 | 2018 | 2018 Geological and Geochemical Program Report on the Pelly Property | Orthophoto - Airphotography, Rock - Geochemistry, Detailed Bedrock Mapping - Geology | ||
| 096998 | 2016 | 2016 Geophysical Report on the Pelly Property | Magnetic - Airborne Geophysics, VTEM - Airborne Geophysics | ||
| 094616 | 2006 | Assessment Report for Exploration Trail establishment, Surveying, Surface Sampling, and Overburden Evaluation on the Goalie Claims Between June 2 and July 19, 2006 | Geotechnical - Studies | ||
| 094236 | 2000 | Finlayson Project Description Report | Environmental Assessment/Impact - Studies, Geotechnical - Studies, Heritage/Archeological - Studies | ||
| 093790 | 1997 | 1997 Summary Report Ground Geophysical and Geochemical, and Diamond Drill Programs on the Puck 1-80 and Cup 1-24 Claims Finlayson Area, Yukon Territory | Diamond - Drilling, Soil - Geochemistry, EM - Ground Geophysics, Magnetics - Ground Geophysics | 5 | 2691 |
| 093652 | 1996 | 1996 Summary Report Airborne and Ground Geophysical, and Diamond Drill Programs Conducted on the Puck 1-80 Claims, Finlayson Lake Area, Yukon Territory | Diamond - Drilling, EM - Ground Geophysics, Magnetics - Ground Geophysics, Line Cutting - Other | 4 | 908.90 |
| 093584 | 1996 | Dighem V Survey for Westmin Resources Limited Wolverine Lake Project Yukon | Electromagnetic - Airborne Geophysics, Magnetic - Airborne Geophysics | ||
| 093414 | 1995 | Assessment Report Describing Prospecting and Geochemical Surveys on the Puck 1-80 Claims | Soil - Geochemistry, Prospecting - Other |
Related References
| Number | Title | Page(s) | Document Type |
|---|---|---|---|
| ARMC016590 | Geochemical map - 105G/8 - Wolverine Lake | Geochemical Map | |
| ARMC016578 | Geology map - 10G/8 - Wolverine Lake | Geoscience Map (Geological - Bedrock) | |
| ARMC017622 | Geochemical map of Wolverine Lake - Cu, Pb, Zn, Mn, Mo.W | Geochemical Map |
| Citations |
|---|
