Ontario Geological Survey
Permanent Link to this Record:
MDI42A11SE00014
| Record Name(s) | Pamour Mine - 1934, Pamour No. 1 - 1984 |
|---|---|
| Related Record Type | Compound |
| Related Record(s) | |
| Record Status | Past Producing Mine Without Reserves or Resources |
| Date Created | 1984-May-01 |
| Date Last Modified | 2023-Aug-03 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Secondary Commodities: Silver, Zinc
Township or Area: Whitney
Latitude: 48° 31' 20.11" Longitude: -81° 7' 13.77"
UTM Zone: 17 Easting: 491103 Northing: 5374356 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42A11SE
Point Location Description: open pit
Location Method: AMIS Site Visit
Access Description: Access to the property is via Hwy 101 east, approximately 8 kilometres northeast of South Porcupine, Ontario. The Pamour property consists of 38 patented mining claims, 3 staked claims and one License of Occupation. Together, the property covers approximately 1 651 acres of mining rights and 1 575 acres of surface rights. Directly adjacent to the Pamour Mine is the Hoyle property that is comprised of 37 patented mining claims and 4 leased claims covering approximately 1 608 acres. The Company has a renewable 10-year lease on that portion of the Hoyle property lying south of the Timiskaming Unconformity where current mining operations are conducted. The lease terms include the payment of a minimum annual rent of $100 000 which is credited against a production royalty being the higher of $0.75 per ton or a 2% net smelter return. In order to renew the lease, which expires in 1999, for a further 10-year term, the Company must spend $1.0 million on exploration and mine one million tons of ore. Both conditions have been satisfied and as a result the Company is entitled to an automatic renewal of the lease. The Company has earned a 51% interest in the portion of the Hoyle property north of the Timiskaming Unconformity, which is not currently in production. (Information taken from the RYO 10K form, 1998).
Land was first staked in the vicinity of the present day Pamour Mine in 1910. Gold was discovered that year in the vicinity of the Pamour Mine by the Three Nations Mining Co. Ltd. and the following year by La Palme Porcupine Mines Ltd., the two fore-runners of the present day Pamour Mine. A small amount of production was achieved from 1911 to 1914, however the property remained idle from 1914 to 1923. 1924: Porcupine Grande Company - tenching, pitting, DD. Various exploration activities were carried out by several mining syndicates until the property was acquired by Noranda in 1935. The Pamour Mine commenced full operations in 1936 and has produced almost 4 million ounces of gold from 44 million tons of ore at a recovered grade of 0.091 oz / ton to the end of 1997 (includes approximately 3 million tons and 229 000 ounces from the Hoyle South Property which is operated under a mining lease agreement with Kinross Gold Corporation). The mine was operated from 1936 to 1986 by Pamour Porcupine Mines Ltd. (a Noranda Inc. sudsidiary). The operation was sold in 1986 to Jimberlana Minerals and subsequently taken over by Giant Resources Limited, both of Australia. A mining lease agreement for the Hoyle Mine was negotiated with Falconbridge Gold Ltd. (now Kinross Gold Corporation) in 1989. Royal Oak Mines Inc. acquired the Pamour and Hallnor mines in 1990, and the contiguous Broulan Reef property was acquired by Royal Oak in 1991. The Pamour open pit mine went back into production in the fall of 2006 as part of the Porcupine Joint Venture. The mine ceased production in 2011.
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Tectonic Assemblage: Timiskaming
Geological Age: Neoarchean Geochronological Age: >2679
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Dec 07, 2005 (R Pressacco) - The Central Tisdale Anticline is to the north of the property. The mine is located on the north limb of an overturned syncline. Pillow tops in the Keewatin metavolcanics and bedding structures in the metasediments locally face south and are overturned. The axis of the syncline dips north at an angle that is slightly less steep than the unconformity, approximately at 70 degrees and strikes approximately N78 degreesE. The south limb of this syncline is interpreted to have been faulted away by the Porcupine-Destor Fault, which is located to the south of the mine property. Aitken (1990) has identified three fold generations at the Pamour No. 1 mine as follows: F1 folds are restricted to the volcanic rocks. They are the oldest known folds and pre-date mineralization. The F1 folding event is interpreted to be related to the formation of the North Tisdale Anticline (Ferguson 1968). F2 folds occur in both volcanic and sedimentary rocks, and also pre-date mineralization. The F2 folds are more prevalent in the area of the 'west end' of the mine (between 2,500 ft west of the No.3 shaft and the Hallnor fault). This folding is much tighter than F1 folds with amplitudes ranging between inches and a hundred feet or more. The youngest F3 folds post-date mineralization, occur in both rock types, and are only weakly developed. Two major post-ore dextral faults, the Hallnor and Pamour faults, strike north to northwest, dip 60 deg east, and offset the stratigraphy by as much as 1 200 feet. There are two systems of less pronounces faults which form a conjugate set. The major set strikes northwest and has dextral displacements of up to 50 feet. Faults of the minor set strike northeast and have sinistral displacements of the same magnitude. These two fault systems appear to be more persistent in the metasedimentary rocks than in the metavolcanic rocks. The faults are interpreted to be extensional as evidenced by down dropping of blocks between sets.
| Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 | Mg-Tholeiitic Basalt | Host |
|---|---|---|---|---|
| Vein | 2 | Quartz | Contains | |
| Terrigenous-Clastic-Unsubdivided | 3 | Greywacke | Host | |
| Ultramafic lava flow-unsubdivided | 4 | Komatiite / Basaltic Komatiite | Near | |
| Conglomerate | 5 | Conglomerate | Host | |
| Siltstone | 6 | Graphitic Argillite | Near |
Dec 07, 2005 (R Pressacco) - The 'North Greywacke' occurs between the unconformity to the north and the conglomerate to the south. It is a discontinuous silty turbidite sequence consisting of intercalated greywackes and slates that show a tendency to pinch and swell in some locations. Stratigraphically, it is located directly above the Timiskaming unconformity and below the Pamour conglomerate. The turbidite sequence in places may reach up to 60 feet in thickness. The Pamour Conglomerate is generally clast supported, polymictic, and unsorted with pebble compositions varying from chert to porphyry. Individual clasts range from pebble to boulder size. The matrix is generally dark and muddy and its proportion to the clasts it hosts varies considerably. The conglomerate unit is lensoidal in shape which is characteristic of a submarine fan depositional origin. It is up to 60 feet thick and thins out at its margins at depth and to the east. The Pamour Conglomerate is harder and more prone to brittle failure than any of the other ore bearing rock types in the area, hence it was more amenable to hydrothermal solutions, and consequently contains more consistent gold mineralization than other rock types. Much of the Pamour Conglomerate has been mined by underground mining methods for decades. The south greywacke lies stratigraphically above the Pamour Conglomerate and is in sharp contact with it. It is a sandy turbidite sequence consisting of a series of well-bedded intercalated slates and medium grained greywacke beds which locally possesses good metasedimentary structures. The unit averages 800 feet in thickness. A second conglomerate unit which occurs in the metasedimentary sequence is a coarse grained, matrix supported rock with a minor amount of pebbles. It grades into an interbedded quartzite-greywacke sequence and is poorly sorted. In places it has minor pyrite and sub-economic gold mineralization. This unit locally contains fuchsitic ultramafic clasts.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Gold | Economic | Ore | ||||
| 2 | Silver | Economic | Ore | ||||
| 3 | Pyrrhotite | Economic | Ore | ||||
| 4 | Sphalerite | Economic | Ore | ||||
| 5 | Galena | Economic | Ore | ||||
| 6 | Arsenopyrite | Economic | Ore | ||||
| 1 | Ankerite | Economic | Gangue | ||||
| 2 | Quartz | Economic | Gangue | ||||
| 3 | Fuchsite | Economic | Gangue | ||||
| 4 | Albite | Economic | Gangue | ||||
| 5 | Sericite | Economic | Gangue | ||||
| Chlorite | Alteration | Unknown | 1 | Medium | Replacement | ||
| Carbonate | Alteration | Carbonatization | 2 | Medium | Replacement | ||
| Quartz | Alteration | Silicification | 3 | Weak | Replacement | ||
| Albite | Alteration | Unknown | 4 | Weak | Replacement | ||
| Sericite | Alteration | Sericitization | 5 | Weak | Replacement |
Dec 07, 2005 (R Pressacco) - There are three distinctive orebody types at the Pamour. In progressive order from north to south they are: 1. Metavolcanic-Hosted Fault-Vein Orebodies (Narrow Vein), 2. Extension-Vein (Bulk) Orebodies, and 3. Metasediment-Hosted Fault-Vein Orebodies (TN Veins), (Aitken 1990). Although the orebody types are genetically and spatially linked, the extension-vein bulk orebodies are the dominant open pit ore type. The bulk type mineralization occurs in the conglomerate and greywackes as sheeted quartz veins or stockwork stringers where the two types of narrow vein structures come together. The resulting 'inverted horseshoe' of orebodies plunge at about 30 degrees to the east. The model is vertically repetitive at about 200 to 400 foot intervals. The majority of gold occurs in two principal modes. The first is as free gold associated with narrow, quartz-ankerite extension-veins along with traces of sphalerite, galena, and locally arsenopyrite. Historically between 15 to 20% of the gold at Pamour Mine is free milling. Pyrite and pyrrhotite also occur within the quartz veins but more commonly occur as disseminated grains in the bleached and altered wallrock. The second mode of gold mineralization is recovered as float concentrate comprised mainly of pyrite associated gold. It occurs as a pervasive, lower grade, disseminated pyrite-gold mineralization associated with the alteration halo surrounding the quartz vein stockworks. Locally, in order of decreasing abundance, arsenopyrite, sphalerite and galena may occur in minor amounts.
Jan 12, 2015 (R Pressacco) - Hydrothermal alteration in the metavolcanic wallrock is characterized by the dominant iron-rich carbonatization and chloritization, less abundant albitization and silicification, and minor sericitization and pyritization. Zonation is asymmetrical and discontinuous around hydrothermal centres, and forms separate inner and outer alteration assemblages. The inner assemblage may be under 100 feet thick, and is characterized by the presence of albite, quartz, pyrite and +/- talc. The outer assemblage is characterized by the reduction of albite and quartz, and the introduction of sericite. It may be several hundreds of feet thick (Aitken 1990). Trace sphalerite, galena and chalcopyrite are confined to quartz veins. Where narrow quartz veins break up into stockwork extension veins (eg. bulk ore hosted by mafic metavolcanic rocks) proximal to impervious lithologic contacts, increased silicification and pyritization of the wallrock occurs. Hydrothermal alteration of the metasediments is more intense, pervasive, and penetrative than that observed in the metavolcanic rocks. Inner zonation in the extension vein bulk ore zones is dominated by quartz + carbonate + albite+sericite + pyrite (Aitken 1990), with minor arsenopyrite, sphalerite, and galena. Wallrock sulphidation of between 3% and 8% occurs around ore zones. Increased pyrite content correlates with increased gold content. Increased amounts of sphalerite and galena, although restricted to quartz vein filling material, also correlate with increased gold content. The outer alteration assemblage is characterized by reduced quartz, albite, pyrite, and sericite, as well as increased carbonate and the introduction of chlorite. Sedimentary fault veins (eg. TN veins) are less extensive in strike length than their extension vein stockwork counterparts. The extent of penetrative alteration is therefore also less in the fault veins. Arsenopyrite becomes more dominant as a penetrative wallroc ksulphide.
| Rank | Classification |
|---|---|
| 1 | Hydrothermal |
| Rank | Characteristic |
|---|---|
| 2 | Stratiform |
| 1 | Vein |
| Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
|---|---|---|---|---|---|---|---|---|---|
| Irregular | 1220 | 45 | 60 | 30 | 90 |
| Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
|---|---|---|---|---|---|---|---|---|---|
| Irregular | 610 | 1 | 610 |
| Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
|---|---|---|---|---|---|---|---|---|---|
| Irregular | 450 | 4.5 | 610 |
| Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
|---|---|---|---|---|---|---|
| Pamour Mine - Reserves | 1997 | Proven + Probable Reserve | 23732100 | RYO 10K form | proven+probable, 1 107 498 contained oz Au | Gold 1.44 Ounce per Ton |
| Pamour Mine - Resources | 1997 | Assay | 45494100 | RYO 10K form | mineral material, includes Nighthawk Mine, 2 435 000 contained oz Au | Gold 1.65 Grams per Tonne |
| Pamour Mine - Resources | 1996 | Assay | 36900000 | RYO 10K form | mined material, 2 386 754 contained oz @ $C527/oz Au($US390/oz) | Gold 2 Ounce per Ton |
| Pamour Mine - Reserves | 1996 | Proven + Probable Reserve | 59568300 | RYO 10K form | proven+probable, 2 697 984 contained ounces | Gold 1.4 Ounce per Ton |
| Year | Tonnes | Commodities | Reference | Comment |
|---|---|---|---|---|
| 2016 | 5113381 |
Gold 8711 Ounces |
OFR6327, p.7 | Grade of 0.635 g/t gold |
| 2011 | 2926622 |
Gold 84357 Ounces |
OFR6274 | @0.897 g/t gold (84 357 ounces) |
| 2010 | 3117410 |
Gold 98921 Ounces |
OFR6264 | @0.987 g/t gold (98 921 ounces) |
| 2009 | 2990445 |
Gold 142204 Ounces |
OFR6247 | @1.479 g/t gold (142 204 ounces) |
| 2008 | 3055196 |
Gold 156116 Ounces |
OFR6235 | @1.589 g/t gold (156 116 ounces) |
| 2007 | 1736560 |
Gold 71321 Ounces |
OFR6203 | @1.277 g/t gold (71 321 ounces) |
| 2006 | 1906145 |
Gold 100448 Ounces |
OFR6203 | @1.793 g/t gold (100,448 ounces) |
| 2005 | 931425 |
Gold 45404 Ounces |
OFR6203 | |
| 1997 | 928181 |
Gold 2064480 Grams |
OFR5985, p.213 | 66 382 recovered ounces Au |
| 1996 | 1004300 |
Gold 2259539 Grams |
OFR5985, p.213 | 72 654 recovered ounces Au |
| 1995 | 1129187 |
Gold 2392336 Grams |
OFR5985, p.213 | 76 924 recovered ounces Au, |
| 1994 | 1162507 |
Gold 2482060 Grams |
OFR5985, p.213 | 79 809 recovered ounces Au |
| 1993 | 1174944 |
Gold 2622041 Grams |
OFR5985, p.213 | 84 310 recovered ounces Au, |
| 1992 | 1102317 |
Gold 3054580 Grams |
OFR5985, p.213 | 98 218 recovered ounces Au, |
| 1991 | 1097966 |
Gold 2856908 Grams |
OFR5985, p.213 | 91 862 recovered ounces Au |
| 1990 | 973013 |
Gold 2360925 Grams |
OFR5985, p.213 | 75 914 recovered ounces Au |
| 1989 | 955296 |
Gold 2166893 Grams |
OFR5985, p.213 | 69 675 recovered ounces Au |
| 1988 | 1193012 |
Gold 2226356 Grams |
OFR5985, p.213 | 71 587 recovered ounces Au |
| 1987 | 1192430 |
Gold 2295958 Grams |
OFR5985, p.213 | 73 825 recovered ounces Au |
| 1986 | 1008684 |
Gold 2070016 Grams |
OFR5985, p.213 | 66 560 recovered ounces Au |
| 1985 | 754062 |
Gold 1624104 Grams |
OFR5985, p.213 | 52 222 recovered ounces Au |
| 1984 | 584327 |
Gold 1260390 Grams |
OFR5985, p.213 | 40 527 recovered ounces Au |
| 1983 | 438103 |
Gold 1197070 Grams |
OFR5985, p.213 | 38 491 recovered ounces Au |
| 1982 | 569948 |
Gold 1530524 Grams |
OFR5985, p.213 | 49 213 recovered ounces Au |
| 1981 | 531453 |
Gold 1340690 Grams |
OFR5985, p.213 | 43 109 recovered ounces Au |
| 1980 | 559394 |
Gold 1548687 Grams |
OFR5985, p.213 | 49 797 recovered ounces Au |
| 1979 | 556355 |
Gold 1783119 Grams |
OFR5985, p.213 | 57 335 recovered ounces Au |
| 1978 | 704294 |
Gold 2028280 Grams |
OFR5985, p.213 | 65 218 recovered ounces Au |
| 1977 | 704294 |
Gold 2025792 Grams |
OFR5985, p.213 | 65 138 recovered ounces Au |
| 1976 | 783307 |
Gold 2541616 Grams |
OFR5985, p.213 | 81 724 recovered ounces Au |
| 1975 | 611131 |
Gold 1993137 Grams |
OFR5985, p.213 | 64 088 recovered ounces Au |
| 1974 | 541120 |
Gold 1794128 Grams |
OFR5985, p.213 | 57 689 recovered ounces Au |
| 1973 | 577850 |
Gold 2281900 Grams |
OFR5985, p.213 | 73 373 recovered ounces Au |
| 1972 | 622800 |
Gold 2795890 Grams |
OFR5985, p.213 | 89 900 recovered ounces Au |
| 1971 | 621000 |
Gold 2643500 Grams |
OFR5985, p.213 | 85 000 recovered ounces Au |
| 1970 | 570600 |
Gold 2481780 Grams |
OFR5985, p.213 | 79 800 recovered ounces Au |
| 1969 | 559800 |
Gold 2687040 Grams |
OFR5985, p.213 | 86 400 recovered ounces Au |
| 1968 | 561600 |
Gold 2220540 Grams |
OFR5985, p.213 | 71 400 recovered ounces Au |
| 1967 | 549000 |
Gold 1990400 Grams |
OFR5985, p.213 | 64 000 recovered ounces Au |
| 1966 | 551250 |
Gold 2005950 Grams |
OFR5985, p.213 | 64 500 recovered ounces Au |
| 1965 | 526050 |
Gneiss 1977960 Grams |
OFR5985, p.213 | 63 600 recovered ounces Au |
| 1964 | 541800 |
Gold 2208100 Grams |
OFR5985, p.213 | 71 000 recovered ounces Au |
| 1963 | 565200 |
Gold 2021500 Grams |
OFR5985, p.213 | 65 000 recovered ounces Au |
| 1962 | 569700 |
Gold 1928200 Grams |
OFR5985, p.213 | 62 000 RECOVERED OUNCES AU |
| 1961 | 583200 |
Gold 1859780 Grams |
OFR5985, p.213 | 59 800 recovered ounces Au |
| 1960 | 581400 |
Gold 1949970 Grams |
OFR5985, p.213 | 62 700 recovered ounces Au |
| 1959 | 573660 |
Gold 1915760 Grams |
OFR5985, p.213 | 61 600 recovered ounces Au |
| 1958 | 582300 |
Gold 1875330 Grams |
OFR5985, p.213 | 60 300 recovered ounces Au |
| 1957 | 565200 |
Gold 1595430 Grams |
OFR5985, p.213 | 51 300 recovered ounces Au |
| 1956 | 557100 |
Gold 1570550 Grams |
OFR5985, p.213 | 50 500 recovered ounces Au |
| 1955 | 572400 |
Gold 1623420 Grams |
OFR5985, p.213 | 52 200 recovered ounces Au |
| 1954 | 573300 |
Gold 1735380 Grams |
OFR5985, p.213 | 55 800 recovered ounces Au |
| 1953 | 564660 |
Gold 1816240 Grams |
OFR5985, p.213 | 58 400 recovered ounces Au |
| 1952 | 549900 |
Gold 1754040 Grams |
OFR5985, p.213 | 56 400 recovered ounces Au |
| 1951 | 523800 |
Gold 1729160 Grams |
OFR5985, p.213 | 55 600 recovered ounces Au |
| 1950 | 544500 |
Gold 1803800 Ounces |
OFR5985, p.213 | 58 000 recovered ounces Au |
| 1949 | 525600 |
Gold 1772700 Grams |
OFR5985, p.213 | 57 000 recovered ounces Au |
| 1948 | 370800 |
Gold 1181800 Grams |
OFR5985, p.213 | 38 000 recovered ounces Au |
| 1947 | 270000 |
Gold 849030 Grams |
OFR5985, p.213 | 27 300 recovered ounces Au |
| 1946 | 348300 |
Gold 1100940 Grams |
OFR5985, p.213 | 35 400 recovered ounces Au |
| 1945 | 376200 |
Gold 1206680 Grams |
OFR5985, p.213 | 38 800 recovered ounces Au |
| 1944 | 423450 |
Gold 1296870 Grams |
OFR5985, p.213 | 41 700 recovered ounces Au |
| 1943 | 472500 |
Gold 1682510 Grams |
OFR5985, p.213 | 54 100 recovered ounces Au |
| 1942 | 517500 |
Gold 1890880 Grams |
OFR5985, p.213 | 60 800 RECOVERED OUNCES AU |
| 1941 | 522000 |
Gold 2079657 Grams |
OFR5985, p.213 | 66 870 recovered ounces Au |
| 1940 | 518400 |
Gold 2201880 Grams |
OFR5985, p.213 | 70 800 recovered ounces Au |
| 1939 | 526860 |
Gold 2192550 Grams |
OFR5985, p.213 | 70 500 recovered ounces Au |
| 1938 | 463680 |
Gold 2923400 Grams |
PRESSACCO (1999) IN PREP. | 94 000 RECOVERED OUNCES AU |
| 1937 | 248580 |
Gold 3514300 |
OFR5985, p.213 | 113 000 recovered ounces Au |
| 1936 | 124380 |
Gold 1819350 Grams |
OFR5985, p.213 | 58 500 ounces Au |
File - Resident Geologist file T-0512
Publication Number: Date:
Author:
Publisher Name:
Location: Timmins RGP office
Map - Geological Compilation of the Timmins Area, Abitibi Greenstone Belt
Publication Number: P3379 Scale: 1:100,000 Date: 1998
Author: Ayer J.A., Trowell N.F.
Publisher Name:
Location:
Publication - Pamour Mine, CIM Jubilee Volume, Vol 1
Publication Number: Page: 558-563 Date: 1948
Author: Price, P. and Bray, R.C.E.
Publisher Name: CIM
Location: Timmins RGO
Book - Gold ’86 Field Guide Abitibi Belt – Timmins to Larder Lake, p. 20-29
Publication Number: N/A Date: 1986
Author: A. Fyon
Publisher Name: GAC
Location: Timmins RGO
Map - Timmins data series, Whitney Township, District of Cochrane
Publication Number: P2123 Scale: 1:15,840 Date: 1981
Author: Hunt D.S., MacRae B.A., Maharaj D.
Publisher Name: Ontario Geological Survey
Location:
Book - Sudbury Timmins Algoma Mineral Program, Project 1: mineral inventory of the Sudbury-Timmins-Sault Ste. Marie region, Ontario
Publication Number: GSC OF 1087 Page: 283 Date: 1985
Author: Rose, D.G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
Map - Structural geology, Whitney Township
Publication Number: P3172 Scale: 1:10,000 Date: 1991
Author: Piroshco D.W., Kettles K.
Publisher Name: Ontario Geological Survey
Location:
Map - Whitney Township, northeast quarter
Publication Number: P0010 Scale: 1:6,000 Date: 1997
Author: Ferguson S.A.
Publisher Name: Ontario Dept. of Mines
Location:
Book - Northern Miner 78-11-09, p. 23
Publication Number: NMINER Date: 1978
Author:
Publisher Name: Northern Miner
Location: Timmins RGO
Book - Northern Miner 80-10-23, Pamour, p. 3
Publication Number: NMINER Date: 1980
Author:
Publisher Name: Northern Miner
Location: Timmins RGO
Book - Northern Miner 80-10-23, p. 3
Publication Number: NMINER Date: 1980
Author:
Publisher Name: Northern Miner
Location: Timmins RGO
Part - The Porcupine gold area
Publication Number: ARV33-02.001 Page: 83 Date: 1998
Author: Burrows A.G.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Gold deposits of Ontario, part 1, districts of Algoma, Cochrane, Kenora, Rainy River, and Thunder Bay
Publication Number: MDC013 Page: 119-120 Date: 1971
Author: Ferguson S.A., Groen H.A., Haynes R.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Mono - Report of Activities 1995, Resident Geologists
Publication Number: OFR5943 Page: 222, 224, 225 Date: 1996
Author: Baker C.L., Fyon J.A., Laderoute D.G., Newsome J.W.
Publisher Name: Ontario Geological Survey
Location:
Article - 1978 report of Northern Regional Geologist and Timmins Resident Geologist
Publication Number: MP084.005 Page: 51-57 Date: 1997
Author: Tihor L.A., Hunt D.S.
Publisher Name: Ontario Geological Survey
Location:
Mono - Preliminary report on the Timmins-Kirkland Lake area, gold deposits file
Publication Number: OFR5467 Date: 1983
Author: Hodgson C.J.
Publisher Name: Ontario Geological Survey
Location:
Article - Timmins Resident Geologist's District - 1988
Publication Number: MP142.012 Page: 231-233, 235 Date: 1997
Author: Luhta L.E., Sangster P.J., Draper D.M., Ireland J.C., Bradshaw M.P., Hamblin C.D.
Publisher Name: Ontario Geological Survey
Location:
Article - Timmins Resident Geologist's District - 1989
Publication Number: MP147.012 Page: 230, 232 Date: 1997
Author: Luhta L.E., Sangster P.J., Ireland J.C., Hamblin C.D., Bradshaw M.P.
Publisher Name: Ontario Geological Survey
Location:
Mono - Special Project: Timmins Ore Deposit Descriptions
Publication Number: OFR5985 Date: 1999
Author: Pressacco R.E.
Publisher Name: Ontario Geological Survey
Location:
Book - The Pamour 1 Minesite Investigation
Publication Number: M.SC. TH Date: 1990
Author: S. Aitken
Publisher Name: Queen's University
Location: Timmins RGO library
Thesis - The Petrology and Geochemistry of Rocks Associated With Gold Deposits, Timmins Area, Ontario
Publication Number: MSc Thesis Date: 1982
Author: Duff, D.
Publisher Name: Laurentian University
Location: Timmins RGO, library
Book - Report II: Pamour #1 Deposits Distribution of primary metavolcanic rock types
Publication Number: Date: 1991
Author: Fan, J. and Kerrich, R.
Publisher Name: University of Saskatchewan, Saskatoon
Location:
MonoMap - Geology and ore deposits of Tisdale Township, District of Cochrane
Publication Number: R058 Date: 1968
Author: Ferguson S.A., Buffam B.S.W., Carter O.F., Griffis A.T., Holmes T.C., Hurst M.E., Jones W.A., Lane H.C., Longley C.S.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of the Timmins area, District of Cochrane
Publication Number: R219 Date: 1982
Author: Pyke D.R.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2016, Resident Geologist Program, Timmins Regional Resident Geologist Report: Timmins and Sault Ste. Marie Districts
Publication Number: OFR6327 Date: 2017
Author: van Hees E., Bousquet P., Pace A., Daniels C.M., Wilson A.C., Samuel A., Walmsley J.
Publisher Name: Ontario Geological Survey
Location:
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