General Information
Secondary Commodities: arsenic, bismuth, copper, zinc, lead, silver, gold
Aliases: Anise, Gull Mineral
Deposit Type(s): Volcanogenic Massive Sulphide (VMS) Kuroko Cu-Pb-Zn
Location(s): 61.627780 N, -132.741670 W
NTS Mapsheet(s): 105F10
Location Comments: .5 Kilometres
Hand Samples Available at YGS: No
Capsule
Work History
Staked as Haydn cl (72700) in Sep/56 by E.M. Neil, probably for Conwest. Unconfirmed reports indicate drilling here in 1956 or 1957. Canol Mines Ltd staked this target in 1968 as part of its large property surrounding the Groundhog showing (Minfile Occurrence # 105F 029)
Restaked as Anise cl 1-64 (YA274) in Jul/76 by a joint venture between Cyprus Anvil Mining Corporation Ltd and Hudson's Bay Oil & Gas Ltd, which performed mapping and geochemical surveys in 1976-78, a Turam survey, bulldozer trenching, and drilled 3 holes (515 m) in 1977.
Restaked as part of a block of 730 Ram cl (YA71576) in Sep/84 by Regional Resources Ltd, which performed an extensive program of mapping, geochemical and geophysical surveys in 1985 and transferred its interest to Fairfield Minerals Ltd in 1986. Fairfield formed a joint venture with Equity Silver Mines Ltd in spring, 1987, and performed mapping, geochemical and geophysical surveys in that year and drilled 15 holes (1 699.56 m), in 1988. Pacific Comox Resources Ltd acquired a 100% working interest in the Ram claims in Jan/93. Fairfield retained a 1% net smelter return interest in the Ram claims.
Around 2000, Pacific Comox divested itself of the Ram claims and the claims reverted to Fairfield (exact process unknown, but probably related to net smelter return interest). In May 2000, Fairfield optioned the claims to Ross River Gold Ltd (a private company). The following month, Ross River optioned the claims as part of a larger claim group, that included the adjoining Tay-LP claims, to Newmont Exploration of Canada Ltd. Between May and Aug/2000 Newmont carried out airborne electromagnetic and magnetic surveys, geological mapping, prospecting, soil sampling and auger soil sampling over the claim block. Newmont continued exploring the property in 2001 but little work was carried out on the Ram claims. In Dec/2001 Newmont dropped the option and returned all the claims to Ross River.
In Feb/2002, Fairfield merged with Almaden Resources Ltd to form a new company, Almaden Minerals Ltd. In May/2002 Ross River Gold Ltd, re-organized and under went a reverse take over with Panamex Resources Inc to emerge as Ross River Minerals Ltd. Later in the year, the company contracted S.J.V. Consultants to reinterpret the 1991 Dighem and 2000 Furgo airborne geophysical surveys using 3-D magnetic inversion software. The company hoped to better target existing anomalies and outline new anomalies. Ross River followed-up the reinterpretation with 11 diamond drill holes (914 m), of which 4 holes (568 m) tested various targets associated with this occurrence.
In 2003 the company continued exploring their claims with prospecting, geological mapping, stream sediment sampling and water analysis. The majority of work was centered over the south end of the property i.e. the area located south of Minfile Occurrence #105G 121. Also in 2003, J. Bond and K. Kennedy of the Yukon Geological Survey studied the surficial geology and ice-flow patterns in the Seagull Creek area.
In 2004 Ross River carried out ground VLF and magnetic geophysical surveys and drilled 9 additional diamond drills holes (1 001.6 m) at the south end of the property. None of the holes were associated with this occurrence.
Capsule Geology
The occurrence is located southwest of the Tintina Fault in the Ketza-Seagull district of the Cassiar Terrane (Platform). The Ketza-Seagull district is underlain by thick (400 m or greater) successions of miogeoclinal clastic, volcanic and carbonate rocks, ranging in age from Upper Proterozoic to Mississippian that were deformed during Mesozoic arc-continental collision, and by mid-Cretaceous intrusions. A series of thrust faults combined with crustal shortening associated with the Seagull Uplift has resulted in older rocks being thrust overtop younger rocks. The Seagull Uplift is thought to be related to uplift above one or more buried Cretaceous intrusions. The Seagull Creek area is known to host at least 19 occurrences consisting of veins, skarns, breccia pipes, disseminated pyrite gossans, stockworks and replacement mantos in volcanics, sediments and carbonates associated with Mississippian age syenite bodies.
The geology of this occurrence is sketchy. The area around the occurrence location is underlain by Upper Cambrian phyllite. Mineralized float was reportedly found in the 1950's in this vicinity. Fairfield Minerals¿ 1985 and 1987 assessment reports show a number of old trenches located in the vicinity of the occurrence, which Canol Mines Ltd referred to as the Gull Mineral zone. The zone is described as a series of trenched mineral occurrences located in the floor of Seagull Valley over a distance of about 1 200 m, that is underlain by very poorly exposed Cambrian to Ordovician phyllite and Devonian to Mississippian volcanic and sedimentary rocks. Float boulders of massive and semi-massive arsenopyrite and pyrite are common. A minor galena-manganosiderite showing hosted by a carbonate horizon was discovered in trench #4, located on the east side of Seagull Creek, approximately 900 m northwest of the occurrence. The best sample from float returned 240 g/t silver and 0.41 g/t gold.
Soil sampling by Canol Mines located several erratic lead-silver anomalies and prospecting located large boulders of massive arsenopyrite-rich float throughout the Anise claims. The source of the float was never located. Fairfield Minerals never found evidence of drilling in the vicinity of the occurrence. It is most likely any drilling undertaken by Canol Mines was located further south on one of the other main showings.
Regional Resources spent 1985 prospecting, soil sampling and re-mapping all of the known mineral showings. Soil sampling outlined small lead-zinc-silver anomalies over the Gull and Lynx mineral zones and larger ones at the Raven, Vole, Trout and Mouse showings. The Lynx mineral zone and the Raven, Vole, Trout and Mouse showings are all located from 2 to 4 km southwest of this occurrence, on the west side of Seagull Creek. All six areas are underlain by Cambrian to Devonian metasediments and carbonate rocks.
In 1987, Fairfield Minerals enlarged the soil grids overlying the Vole, Trout and Mouse showings in hope of better defining possible drill targets. The company also changed their focus towards locating veins, stockworks and replacement bodies that carried anomalous gold values. Prospecting around the Trout showing (located approximately 4 km southwest of the occurrence), located a quartz vein containing massive pyrrhotite-pyrite-arsenopyrite. A 3 m chip sample returned an averaged of 0.6% lead, 1.4% zinc, 155 g/t silver and 5.3% arsenic. Prospecting also discovered numerous quartz boulders containing 30 to 75% pyrite and 3 to 20% arsenopyrite that returned from 0.07 to 12.4 g/t gold and up to 433.7 g/t silver. Four 1988 drill holes which tested the showing and associated geophysical anomalies, intersected pyrrhotite-pyrite-arsenopyrite mineralization of similar grade and style, over a strike length of 90 m
Diamond drilling on the Vole showing located 3.4 km southwest of the occurrence intersected 2 to 4 m widths of mineralization similar to that observed at the Trout showing. Four of five drill holes collared on the Mouse zone (located approximately 1.8 km south of this occurrence), intersected massive and disseminated magnetite skarn.
Following the completion of the 1988 drilling program the Ram claims remained dormant and most of the outlying claims were allowed to lapse. By the time Ross River Gold and subsequently Newmont Exploration assumed the option in 2000, the property was reduced to 69 claims centered over Seagull Creek.
Soil sampling by Newmont outlined a 800 by up to 200 m wide area near the Vole showing defined by frequent > 10 ppb gold results, situated within a larger area defined by > 250 ppm arsenic. Bismuth, silver, lead and antimony values are also anomalous. The company also identified a 1 600 by 700 m wide gold-bismuth anomaly called the Wolf anomaly located on the east side of Seagull Creek near Minfile Occurrence #105F 023. This anomaly returned values up to 250 ppb gold and 53.9 ppm bismuth. Two samples collected by power auger from this anomaly returned 155 and 435 ppm gold. The latter sample was collected from the north side of the anomaly while the former was collected from the south side.
The airborne geophysical reinterpretation outlined several broad trends. One trend is thought to represent a series of depth limited sources, most likely skarn deposits. A second trend is thought to represent buried intrusives. Still another trend is thought to represent the trend of the Seagull Fault. The contractor strongly suggested that all identified targets be verified on the ground before drilling was attempted.
Of the four drill holes collared in the vicinity of this occurrence only one hole, (hole 9) intersected anomalous mineralization. The hole which tested a EM conductor, intersected 20.55 m of minor quartz veining containing pyrite-marcasite +/- arsenopyrite mineralization. A 0.3 m intersection within this zone assayed 0.97 g/t gold. The other three holes did not return any significant assays.
Limited prospecting and geochemical sampling carried out in 2003 in the vicinity of this occurrence returned a few anomalous results, none of which identified new targets. Field work by Kennedy and Bond (2004) determined that glacial flow in the Seagull Creek area was to the north, up-valley, in the opposite direction to what had previously been believed. These results have a significant bearing on the interpretation of soil geochemical anomalies and the potential of known mineralized occurrences in the area. Ross River hopes to use this data to improve their search results.
All of the 2004 drill holes and geophysical surveys were carried out in the southern half of the property (i.e. Tay-LP claims).
References
ALMADEN MINERALS LTD, Apr/2003. Web Site: www.almadenminerals.com/
CANADIAN MINES HANDBOOK 2000-01. p.150. (Indicates return of Ram claims to Fairfield Minerals Ltd).
CYPRUS ANVIL MINING CORP., Jan/77. Assessment Reports #090175 by P. Dean.
CYPRUS ANVIL MINING CORP., Jun/77. Assessment Reports #090200 by P. Dean.
FAIRFIELD MINERALS LTD, Sept/87. Assessment Report #092096 by J.J. Hylands.
FAIRFIELD MINERALS LTD, Jan/89. Assessment Report #092611 by J.J. Hylands.
GEORGE CROSS NEWSLETTER, 18 Jan/93.
KENNEDY, K.E. AND BOND, J.D., 2004. Evidence for a late-McConnell readvance of the Cassiar Lobe in Seagull Creek, Pelly Mountains, central Yukon. In: Yukon exploration and Geology 2003, D.S. Emond and L.L. Lewis (eds.), Yukon Geological Survey.
MINERAL INDUSTRY REPORT, 1976, p. 197-198; 1977, p. 83.
NEWMONT EXPLORATION OF CANADA LTD, Jan/2001. Assessment Report #094189 by A.T. Montgomery and M.A. Stammers.
PANAMEX RESOURCES INC, Jul/2001. Preliminary Exchange Offering Prospectus. (Outlines reverse take over and re-organization of Ross River Gold Ltd).
REGIONAL RESOURCES LTD, Jan/86. Assessment Report #091768 by M.A. Stammers.
ROSS RIVER MINERALS LTD, Jun/2003. Assessment Report #094416 by R.S Tolbert.
ROSS RIVER MINERALS LTD, Mar/2004. Assessment Report #094445 by R.S. Tolbert.
ROSS RIVER MINERALS LTD, Apr/2003; Jun/2005. Web Site: www.rossriverminerals.com/
ROSS RIVER MINERALS LTD, Press Release: 14 Apr/2002.
YUKON EXPLORATION 1987, p. 154; 1988, p. 75.
YUKON EXPLORATION & GEOLOGY 2001, p. 9-10; 2002, p. 9-10, 25, 26; 2003, p. 13, 26; 2004, p. 12-13, 32, 33.
YUKON GEOLOGY AND EXPLORATION 1979-80, p. 175.
Staked as Haydn cl (72700) in Sep/56 by E.M. Neil, probably for Conwest. Unconfirmed reports indicate drilling here in 1956 or 1957. Canol Mines Ltd staked this target in 1968 as part of its large property surrounding the Groundhog showing (Minfile Occurrence # 105F 029)
Restaked as Anise cl 1-64 (YA274) in Jul/76 by a joint venture between Cyprus Anvil Mining Corporation Ltd and Hudson's Bay Oil & Gas Ltd, which performed mapping and geochemical surveys in 1976-78, a Turam survey, bulldozer trenching, and drilled 3 holes (515 m) in 1977.
Restaked as part of a block of 730 Ram cl (YA71576) in Sep/84 by Regional Resources Ltd, which performed an extensive program of mapping, geochemical and geophysical surveys in 1985 and transferred its interest to Fairfield Minerals Ltd in 1986. Fairfield formed a joint venture with Equity Silver Mines Ltd in spring, 1987, and performed mapping, geochemical and geophysical surveys in that year and drilled 15 holes (1 699.56 m), in 1988. Pacific Comox Resources Ltd acquired a 100% working interest in the Ram claims in Jan/93. Fairfield retained a 1% net smelter return interest in the Ram claims.
Around 2000, Pacific Comox divested itself of the Ram claims and the claims reverted to Fairfield (exact process unknown, but probably related to net smelter return interest). In May 2000, Fairfield optioned the claims to Ross River Gold Ltd (a private company). The following month, Ross River optioned the claims as part of a larger claim group, that included the adjoining Tay-LP claims, to Newmont Exploration of Canada Ltd. Between May and Aug/2000 Newmont carried out airborne electromagnetic and magnetic surveys, geological mapping, prospecting, soil sampling and auger soil sampling over the claim block. Newmont continued exploring the property in 2001 but little work was carried out on the Ram claims. In Dec/2001 Newmont dropped the option and returned all the claims to Ross River.
In Feb/2002, Fairfield merged with Almaden Resources Ltd to form a new company, Almaden Minerals Ltd. In May/2002 Ross River Gold Ltd, re-organized and under went a reverse take over with Panamex Resources Inc to emerge as Ross River Minerals Ltd. Later in the year, the company contracted S.J.V. Consultants to reinterpret the 1991 Dighem and 2000 Furgo airborne geophysical surveys using 3-D magnetic inversion software. The company hoped to better target existing anomalies and outline new anomalies. Ross River followed-up the reinterpretation with 11 diamond drill holes (914 m), of which 4 holes (568 m) tested various targets associated with this occurrence.
In 2003 the company continued exploring their claims with prospecting, geological mapping, stream sediment sampling and water analysis. The majority of work was centered over the south end of the property i.e. the area located south of Minfile Occurrence #105G 121. Also in 2003, J. Bond and K. Kennedy of the Yukon Geological Survey studied the surficial geology and ice-flow patterns in the Seagull Creek area.
In 2004 Ross River carried out ground VLF and magnetic geophysical surveys and drilled 9 additional diamond drills holes (1 001.6 m) at the south end of the property. None of the holes were associated with this occurrence.
Capsule Geology
The occurrence is located southwest of the Tintina Fault in the Ketza-Seagull district of the Cassiar Terrane (Platform). The Ketza-Seagull district is underlain by thick (400 m or greater) successions of miogeoclinal clastic, volcanic and carbonate rocks, ranging in age from Upper Proterozoic to Mississippian that were deformed during Mesozoic arc-continental collision, and by mid-Cretaceous intrusions. A series of thrust faults combined with crustal shortening associated with the Seagull Uplift has resulted in older rocks being thrust overtop younger rocks. The Seagull Uplift is thought to be related to uplift above one or more buried Cretaceous intrusions. The Seagull Creek area is known to host at least 19 occurrences consisting of veins, skarns, breccia pipes, disseminated pyrite gossans, stockworks and replacement mantos in volcanics, sediments and carbonates associated with Mississippian age syenite bodies.
The geology of this occurrence is sketchy. The area around the occurrence location is underlain by Upper Cambrian phyllite. Mineralized float was reportedly found in the 1950's in this vicinity. Fairfield Minerals¿ 1985 and 1987 assessment reports show a number of old trenches located in the vicinity of the occurrence, which Canol Mines Ltd referred to as the Gull Mineral zone. The zone is described as a series of trenched mineral occurrences located in the floor of Seagull Valley over a distance of about 1 200 m, that is underlain by very poorly exposed Cambrian to Ordovician phyllite and Devonian to Mississippian volcanic and sedimentary rocks. Float boulders of massive and semi-massive arsenopyrite and pyrite are common. A minor galena-manganosiderite showing hosted by a carbonate horizon was discovered in trench #4, located on the east side of Seagull Creek, approximately 900 m northwest of the occurrence. The best sample from float returned 240 g/t silver and 0.41 g/t gold.
Soil sampling by Canol Mines located several erratic lead-silver anomalies and prospecting located large boulders of massive arsenopyrite-rich float throughout the Anise claims. The source of the float was never located. Fairfield Minerals never found evidence of drilling in the vicinity of the occurrence. It is most likely any drilling undertaken by Canol Mines was located further south on one of the other main showings.
Regional Resources spent 1985 prospecting, soil sampling and re-mapping all of the known mineral showings. Soil sampling outlined small lead-zinc-silver anomalies over the Gull and Lynx mineral zones and larger ones at the Raven, Vole, Trout and Mouse showings. The Lynx mineral zone and the Raven, Vole, Trout and Mouse showings are all located from 2 to 4 km southwest of this occurrence, on the west side of Seagull Creek. All six areas are underlain by Cambrian to Devonian metasediments and carbonate rocks.
In 1987, Fairfield Minerals enlarged the soil grids overlying the Vole, Trout and Mouse showings in hope of better defining possible drill targets. The company also changed their focus towards locating veins, stockworks and replacement bodies that carried anomalous gold values. Prospecting around the Trout showing (located approximately 4 km southwest of the occurrence), located a quartz vein containing massive pyrrhotite-pyrite-arsenopyrite. A 3 m chip sample returned an averaged of 0.6% lead, 1.4% zinc, 155 g/t silver and 5.3% arsenic. Prospecting also discovered numerous quartz boulders containing 30 to 75% pyrite and 3 to 20% arsenopyrite that returned from 0.07 to 12.4 g/t gold and up to 433.7 g/t silver. Four 1988 drill holes which tested the showing and associated geophysical anomalies, intersected pyrrhotite-pyrite-arsenopyrite mineralization of similar grade and style, over a strike length of 90 m
Diamond drilling on the Vole showing located 3.4 km southwest of the occurrence intersected 2 to 4 m widths of mineralization similar to that observed at the Trout showing. Four of five drill holes collared on the Mouse zone (located approximately 1.8 km south of this occurrence), intersected massive and disseminated magnetite skarn.
Following the completion of the 1988 drilling program the Ram claims remained dormant and most of the outlying claims were allowed to lapse. By the time Ross River Gold and subsequently Newmont Exploration assumed the option in 2000, the property was reduced to 69 claims centered over Seagull Creek.
Soil sampling by Newmont outlined a 800 by up to 200 m wide area near the Vole showing defined by frequent > 10 ppb gold results, situated within a larger area defined by > 250 ppm arsenic. Bismuth, silver, lead and antimony values are also anomalous. The company also identified a 1 600 by 700 m wide gold-bismuth anomaly called the Wolf anomaly located on the east side of Seagull Creek near Minfile Occurrence #105F 023. This anomaly returned values up to 250 ppb gold and 53.9 ppm bismuth. Two samples collected by power auger from this anomaly returned 155 and 435 ppm gold. The latter sample was collected from the north side of the anomaly while the former was collected from the south side.
The airborne geophysical reinterpretation outlined several broad trends. One trend is thought to represent a series of depth limited sources, most likely skarn deposits. A second trend is thought to represent buried intrusives. Still another trend is thought to represent the trend of the Seagull Fault. The contractor strongly suggested that all identified targets be verified on the ground before drilling was attempted.
Of the four drill holes collared in the vicinity of this occurrence only one hole, (hole 9) intersected anomalous mineralization. The hole which tested a EM conductor, intersected 20.55 m of minor quartz veining containing pyrite-marcasite +/- arsenopyrite mineralization. A 0.3 m intersection within this zone assayed 0.97 g/t gold. The other three holes did not return any significant assays.
Limited prospecting and geochemical sampling carried out in 2003 in the vicinity of this occurrence returned a few anomalous results, none of which identified new targets. Field work by Kennedy and Bond (2004) determined that glacial flow in the Seagull Creek area was to the north, up-valley, in the opposite direction to what had previously been believed. These results have a significant bearing on the interpretation of soil geochemical anomalies and the potential of known mineralized occurrences in the area. Ross River hopes to use this data to improve their search results.
All of the 2004 drill holes and geophysical surveys were carried out in the southern half of the property (i.e. Tay-LP claims).
References
ALMADEN MINERALS LTD, Apr/2003. Web Site: www.almadenminerals.com/
CANADIAN MINES HANDBOOK 2000-01. p.150. (Indicates return of Ram claims to Fairfield Minerals Ltd).
CYPRUS ANVIL MINING CORP., Jan/77. Assessment Reports #090175 by P. Dean.
CYPRUS ANVIL MINING CORP., Jun/77. Assessment Reports #090200 by P. Dean.
FAIRFIELD MINERALS LTD, Sept/87. Assessment Report #092096 by J.J. Hylands.
FAIRFIELD MINERALS LTD, Jan/89. Assessment Report #092611 by J.J. Hylands.
GEORGE CROSS NEWSLETTER, 18 Jan/93.
KENNEDY, K.E. AND BOND, J.D., 2004. Evidence for a late-McConnell readvance of the Cassiar Lobe in Seagull Creek, Pelly Mountains, central Yukon. In: Yukon exploration and Geology 2003, D.S. Emond and L.L. Lewis (eds.), Yukon Geological Survey.
MINERAL INDUSTRY REPORT, 1976, p. 197-198; 1977, p. 83.
NEWMONT EXPLORATION OF CANADA LTD, Jan/2001. Assessment Report #094189 by A.T. Montgomery and M.A. Stammers.
PANAMEX RESOURCES INC, Jul/2001. Preliminary Exchange Offering Prospectus. (Outlines reverse take over and re-organization of Ross River Gold Ltd).
REGIONAL RESOURCES LTD, Jan/86. Assessment Report #091768 by M.A. Stammers.
ROSS RIVER MINERALS LTD, Jun/2003. Assessment Report #094416 by R.S Tolbert.
ROSS RIVER MINERALS LTD, Mar/2004. Assessment Report #094445 by R.S. Tolbert.
ROSS RIVER MINERALS LTD, Apr/2003; Jun/2005. Web Site: www.rossriverminerals.com/
ROSS RIVER MINERALS LTD, Press Release: 14 Apr/2002.
YUKON EXPLORATION 1987, p. 154; 1988, p. 75.
YUKON EXPLORATION & GEOLOGY 2001, p. 9-10; 2002, p. 9-10, 25, 26; 2003, p. 13, 26; 2004, p. 12-13, 32, 33.
YUKON GEOLOGY AND EXPLORATION 1979-80, p. 175.
Location Map
Last Updated: Sep 13, 2018
Work History
| Year | Work Type | Comment |
|---|---|---|
| 2004 | Other: Prospecting | Only minor prospecting carried out near this occurrence. |
| 2003 | Geochemistry: Silt | |
| 2003 | Geochemistry: Water | |
| 2003 | Other: Prospecting | |
| 2002 | Drilling: Diamond | Four holes, 568 m. Part of larger drill program carried out on property. |
| 2000 | Airborne Geophysics: Electromagnetic | Also magnetic survey. |
| 2000 | Geochemistry: Rock | |
| 2000 | Geochemistry: Soil | |
| 2000 | Geology: Bedrock Mapping | |
| 1988 | Drilling: Diamond | Fifteen holes, 1,699.56 m. Collared to south on Trout, Vole and Mouse zones. |
| 1988 | Geochemistry: Soil | |
| 1988 | Geology: Bedrock Mapping | |
| 1987 | Geochemistry: Soil | |
| 1987 | Ground Geophysics: IP | Also magnetic, VLF-EM, and HLEM surveys. Conducted as a test program. |
| 1985 | Geochemistry: Soil | |
| 1985 | Geology: Bedrock Mapping | |
| 1985 | Trenching: Hand | |
| 1978 | Geochemistry: Soil | |
| 1978 | Geology: Bedrock Mapping | |
| 1977 | Drilling: Diamond | Three holes, 515 m. |
| 1977 | Geochemistry: Soil | |
| 1977 | Geology: Bedrock Mapping | |
| 1977 | Ground Geophysics: EM | Turam survey. |
| 1977 | Trenching: Mechanical | |
| 1976 | Geochemistry: Soil | |
| 1976 | Geology: Bedrock Mapping | |
| 1976 | Other: Prospecting |
Regional Geology - Terrane
Group: Ancestral North America
Affinity: W Laurentia
Name: Cassiar
Realm: Laurentia
Regional Geology - Bedrock
Supergroup:
Group/Suite: Kechika
Formation:
Member:
Terrane: Cassiar
Period Max: Cambrian
Age Max: 500 MA
Period Min: Ordovician
Age Min: 472 MA
Rock Major: slate/phyllite/limestone
Rock Minor: dolostone/basalt/tuff/flows/sills
Reference: Tempelman-Kluit (1977) - GSC OF 486
Geological Unit (1M): COK
Geological Unit (250K): COK1
Assessment Reports that overlap occurrence
| Report Number | Year | Title | Worktypes | Holes Drilled | Meters Drilled |
|---|---|---|---|---|---|
| 095218 | 2010 | 2009 Diamond Drilling Program | Diamond - Drilling, Diamond - Drilling | 10 | 1868 |
| 094416 | 2002 | 2002 Diamond Drilling Assessment Report On the Tay-LP Project | All Weather Road - Development, Surface, Reclamation - Development, Surface, Diamond - Drilling, Drill Core - Geochemistry | 11 | 910.92 |
| 094264 | 2001 | 2001 Diamond Drilling Assessment Report on the Tay-LP and Ram Claim Group | Diamond - Drilling, Bedrock Mapping - Geology | 6 | |
| 094189 | 2000 | 2000 Geological, Geochemical & Geophysical Assessment Report on the Ram Project | Electromagnetic - Airborne Geophysics, Magnetic - Airborne Geophysics, Auger - Drilling, Rock - Geochemistry, Soil - Geochemistry, Bedrock Mapping - Geology, Prospecting - Other | 10 | |
| 090200 | 1977 | Geological, Geochemical and Geophysical Report, Anise Claim Group | Soil - Geochemistry, Bedrock Mapping - Geology, EM - Ground Geophysics, Magnetics - Ground Geophysics | ||
| 090175 | 1976 | Geochemical Exploration Report, Anise Claim Group | Soil - Geochemistry |
Related References
| Number | Title | Page(s) | Document Type |
|---|---|---|---|
| ARMC009273 | Geology map - Fig. 4-3 - Pass Peak - Pelly project | Geoscience Map (Geological - Bedrock) | |
| ARMC009274 | Claim map and proposed DDH site - Pelmac project - Anise claims | Geoscience Map (General) | |
| ARMC009275 | Location map - Pelmac project - Anise claims | Geoscience Map (General) | |
| ARMC009276 | Grid map - Pelmac project - Anise claims | Geoscience Map (General) | |
| ARMC009277 | Turam electromagnetic survey - Pelmac project - Anise claims - Figure 11 | Geophysical Map | |
| ARMC009278 | Geochemical results map - 105F-10 - Seagull Valley detail area - Pelly project | Geochemical Map | |
| ARMC009279 | Geochemical results map - 105F-10 - Seagull Valley detail area - Pelly project | Geochemical Map | |
| ARMC009280 | Geology map - Anise claims - Figure 3 | Geoscience Map (Geological - Bedrock) | |
| ARMC014318 | Regional geology - Pelly Mountains - Pelmac project - Field work completed from July - September 1980 | Report | |
| ARMC014316 | NTS sheet 105F - Quiet Lake with field notations | Geoscience Map (General) | |
| ARMC014433 | 1980 field report - Anise claim group - Field work done from August 16 to September17, 1980 | Report | |
| ARMC014313 | Pelly project summary report: 1978 - Watson Lake mining district, Yukon Territory - Field work done during the period: June 12 - August 30, 1978 | Report | |
| ARMC014233 | Claims map drawn on NTS sheet 105F - Quiet Lake | Geoscience Map (General) | |
| ARMC020394 | Field notes - Pelly Mountains - Anise, Howru, Vangorda, Eros claims | Miscellaneous Company Documents | |
| ARMC014430 | Diamond drill core log and diamond drill record - Pelmac - Anise claim - 80-A-01 | Drill Logs | |
| ARMC014431 | Diamond drill core log and diamond drill record - Pelmac - Anise claim - 80-A-02 | Drill Logs | |
| ARMC014432 | Diamond drill core log and diamond drill record - Pelmac - Anise claim - 80-A-03 | Drill Logs |
| Citations |
|---|
Drill Core at YGS Core Library
| Number | Property | Year Drilled | Core Size | Photos | Data |
|---|---|---|---|---|---|
| 80-A-01 | Haydn | 1980 | BQ | 16 | 1 |
| 80-A-02 | Haydn | 1980 | BQ | 14 | 1 |
| 80-A-03 | Haydn | 1980 | BQ | 12 | 1 |
