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Ontario Geological Survey
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MDI32D05NW00158
Record Name(s) | Iris Mine - 1929, McDonald Claim (7324) - 1918, A.H. Perron - 1981, Perrex Resources Inc. - 1986, Alberta Gold Explorations Corp. - 1997, Iris Gold Mines Ltd. - 1929 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Developed Prospect With Reported Reserves or Resources |
Date Created | 1983-Dec-15 |
Date Last Modified | 2024-May-01 |
Created By | |
Revised By |
Primary Commodities: Gold
Secondary Commodities: Tungsten
Township or Area: Harker
Latitude: 48° 27' 19.66" Longitude: -79° 46' 35.09"
UTM Zone: 17 Easting: 590467 Northing: 5367648 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 32D05NW
Point Location Description: adit
Location Method: AMIS Site Visit
Access Description: Access to the claims is from the west via the Harker-Holloway Mineral Access Road and from the north via dirt roads east of Matheson which are accessed by Highway 101.
1918: McDonald Claim - stripping, sampling. 1929-1947: Iris Gold Mines Ltd. - mapping, stripping, trenching, pitting and sampling. 1981-1987: A.H. Perron (Perrex Resources Inc.) - airborne geophysics, VLF EM and magnetometer surveys; humus sampling, geological survey; DD-5000m (east of and on eastern contact of albite syenite plug), stripping, trenching. 1997-2002: Perrex Resources Inc. and Alberta Gold Exploration Corp. - property optioned, IP survey, EM and magnetometer surveys, DD-47-30,988 ft, exploration ramp blasted for exploration; exploration ramp prepared; mapping, ground geophysics. 2004-2012: Tiger Gold Exploration Corp. - ground geophysics, trenching, blasting
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
KL-0012/W8808.366 | 32D12SW5054 | 32D12SW5054 |
KL-2230/2.4529 | 32D05NW0094 | 32D05NW0094 |
KL-2230/ 2.6067 | 32D05NW0087 | 32D05NW0087 |
63.4571/OM84-214 | 32D05NW0018 | 32D05NW0018 |
2.14728 | 32D05NW0052 | 32D05NW0052 |
KL-3430/OM91-193 | 32D05NW0121 | 32D05NW0121 |
KL2210/2.8657 | 32D12SW0066 | 32D12SW0066 |
KL-3170/ 77 | 32D05NW9406 | 32D05NW9406 |
KL-4935/2.21402 | 32D05NW2097 | 32D05NW2097 |
2.17953 | 32D05NW0175 | 32D05NW0175 |
59 | 32D05NW0383 | 32D05NW0383 |
KL-4825/2.20459 | 32D05NW2074 | 32D05NW2074 |
KL-4847/2.20595 | 32D05NW2076 | 32D05NW2076 |
KL-4865/2.20749 | 32D05NW2078 | 32D05NW2078 |
KL-4853/2.20655 | 32D05NW2092 | 32D05NW2092 |
KL-4838/2.20544 | 32D05NW2093 | 32D05NW2093 |
KL-4845/2.20624 | 32D05NW2094 | 32D05NW2094 |
2.22331 | 32D05NW2106 | 32D05NW2106 |
2.22578 | 32D05NW2107 | 32D05NW2107 |
2.22474 | 32D05NW2109 | 32D05NW2109 |
2.22646 | 32D05NW2110 | 32D05NW2110 |
2.22665 | 32D05NW2111 | 32D05NW2111 |
2.22547 | 32D05NW2112 | 32D05NW2112 |
2.22806 | 32D05NW2120 | 32D05NW2120 |
2.28258 | 32D05NW2169 | 32D05NW2169 |
KL-4937/2.21333 | 32D05NW2096 | 32D05NW2096 |
KL-6729/2.53416 | 20000008636 | 20000008636 |
KL-2230/ 2.5755 | 32D05NW0092 | 32D05NW0092 |
KL-0012/ 2.14728 | 32D05NW0052 | 32D05NW0052 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Geological Age: Mesoarchean
Metamorphism Grade: Greenschist
Rock Type | Rank | Composition | Texture | Relationship | Diabase | 1 | Diabase | Near |
---|---|---|---|---|
Lamprophyre-Unsubdivided | 2 | Near | ||
Pyroxenite | 3 | Pyroxenite | Near | |
Syenite | 4 | Pyrite-Bearing | Host | |
Mafic pillowed flow | 5 | Basalt | Pillowed | Host |
Terrigenous-Clastic-Unsubdivided | 6 | Interflow Sediments | Near | |
Ironstone-unsubdivided | 6 | Near | ||
Vein | 7 | Quartz | Contains | |
Felsic lava flow-unsubdivided | 8 | Rhyolite | Host |
Jun 24, 2015 (A Wilson) - Gold is hosted in a coarse-grained, pyritic syenite intrusion that is cut by north-striking quartz veins, which also contain gold and scheelite. An exploration ramp, 10 by 10 by 500 feet in length, provides underground access to the deposit. The Iris stock is a multiphased intrusion with 1) hornblendite and/or clinopyroxenite around the east and south periphery; 2) medium-grained syenite and/or monzonite mostly along the south part of the intrusion; and 3) coarse-grained syenite along the north and west flanks. The coarse-grained syenite is composed of centimetre-size perthite and anti-perthite crystals that comprise between 80 and 90% of the rock. Strongly chloritized mafic phenocrysts and trace amounts to 3% pyrite comprise the remainder of this phase. Only the coarse-grained syenite contains appreciable gold. Geochemistry of this phase indicates that the syenite is highly sodic and probably a result of late sodium-rich volatiles in the magma. The Iris deposit is 7 km south of the PDDZ and is not associated with any major structural features.
Dec 07, 2005 (R Degagne) - Bedrock in the area consists mainly of largely glacial drift covered weakly metamorphosed (greenschist or lower metamorphic facies) subaqueously deposited tholeiitic basaltic flow and related rocks of the (Archean) Kinojevis Group (Baker et al. 1982; Jensen 1982; Jensen and Langford 1985; Jensen and Baker 1986; Johnstone and Steele 1989; McClenaghan et al. 1988, 1987; Steele 1988). These rocks form a monoclinal succession which is uniformly northeast striking, steeply south dipping, and south facing. The Mine is about 4,000 m stratigraphically beneath (northwest of) the upper Kinojevis Group contact. At least two narrow (less than about 100 m wide) rhyolite horizons are intercalated with basalt in the deposit area, and interflow sediment (including iron formation) have been identified on claim nos. 802701 and 802954 (assessment files, Resident Geologist's Office, Kirkland Lake). Intrusive rocks in the area include a small albite syenitic plug and associated syenitic dikes which intrude basaltic and rhyolitic flow and related rocks; a pyroxenitic body located immediately south of and in contact with the syenite plug; narrow, often flow-contact controlled lamprophyre dikes (Satterly 1952); and a narrow, north northwest striking diabase dike.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Gold | Economic | Ore | ||||
2 | Pyrite | Economic | Ore | ||||
3 | Chalcopyrite | Economic | Ore | ||||
4 | Galena | Economic | Ore | ||||
5 | Scheelite | Economic | Ore | ||||
6 | Specularite | Economic | Ore | ||||
1 | Quartz | Economic | Gangue | ||||
2 | Feldspar | Economic | Gangue | ||||
4 | Dolomite | Economic | Gangue | ||||
Sericite | Alteration | Sericitization | 1 | Unknown | Disseminated | ||
Epidote | Alteration | Saussuritization | 2 | Unknown | Disseminated | ||
Chlorite | Alteration | Chloritic | 3 | Unknown | Disseminated |
Jun 24, 2015 (A Wilson) - Samples collected from the McDonald Claim in 1919 returned assays of $7.60 and $8.40. Highly anomalous gold values up to 0.40 oz/t Au were obtained from pyritic quartz and and rhyolite. Samples collected from a vein in the #1 pit (claim 9735) returned assays of $10.15 Au over 1.7 ft; $9.45 Au over 2.0 ft and $2.80 Au over 1.9 ft. Channel samples from the #2 pit returned values under $1.40. Samples from the #2 vein (claim L8650) assayed up to $1.35 Au. The #2 vein has been traced by trenching for more than 1000 ft. The No. 3 vein is located on the line between mining claim L9920 and L7308, two pits were put down on the vein with the best assay value being $3.15 Au over 14 ft.
Dec 07, 2005 (R Degagne) - Analyses*: Au ppb, Ag ppm, Cu ppm, Pb ppm, Zn ppm, Mo ppm, As ppm, Ba ppm, Sample AB-85-42: <0.01* Au ppb, <0.10* Ag ppm, 24 Cu ppm, <10 Pb ppm, 190 Zn ppm, --- Mo ppm, 4.5 As ppm, 30 Ba ppm, Sample AB-85-43: <0.01* Au ppb, <0.10* Ag ppm, 6 Cu ppm, <10 Pb ppm, 72 Zn ppm, --- Mo ppm, 2.0 As ppm, 40 Ba ppm, Sample AB-85-43a: <0.01* Au ppb, 0.16* Ag ppm, 7 Cu ppm, <10 Pb ppm, 65 Zn ppm, --- Mo ppm, 3.0 As ppm, 50 Ba ppm, Sample AB-85-44: <0.01* Au ppb, <0.10* Ag ppm, 18 Cu ppm, 59 Pb ppm, 36 Zn ppm, --- Mo ppm, 25 As ppm, 120 Ba ppm, Sample AB-85-45: <0.01* Au ppb, <0.10* Ag ppm, 18 Cu ppm, <10 Pb ppm, 140 Zn ppm, --- Mo ppm, 5.5 As ppm, 190 Ba ppm, Sample AB-85-45: <0.01* Au ppb, 0.42* Ag ppm, 6 Cu ppm, <10 Pb ppm, 215 Zn ppm, --- Mo ppm, <1 As ppm, 200 Ba ppm, Sample AB-85-45b: <0.01* Au ppb, 0.11* Ag ppm, 6 Cu ppm, <10 Pb ppm, 111 Zn ppm, --- Mo ppm, 1.5 As ppm, 200 Ba ppm, Sample AB-87-156: 205 Au ppb, 4.1 Ag ppm, 139 Cu ppm, 30 Pb ppm, 15 Zn ppm, <10 Mo ppm, --- As ppm, --- Ba ppm, Sample AB-87-157: 617 Au ppb, 33.25 Ag ppm, 3340 Cu ppm, 5400 Pb ppm, 500 Zn ppm, <10 Mo ppm, --- As ppm, --- Ba ppm, Sample AB-87-201: 516 Au ppb, nil Ag ppm, 10 Cu ppm, <10 Pb ppm, 8 Zn ppm, <10 Mo ppm, <10 As ppm, --- Ba ppm.
Rank | Classification |
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1 | Hydrothermal |
Rank | Characteristic |
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2 | Disseminated |
3 | Sheared |
1 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
---|---|---|---|---|---|---|---|---|---|
Unknown | 914 | 1.5 | 65 |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
---|---|---|---|---|---|---|---|---|---|
Tabular |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
---|---|---|---|---|---|---|---|---|---|
Tabular |
Date: Jun 14, 1989
Geologist: R Degagne
Notes: The No.1 occurrence is reported to have consisted of a 5 foot wide pyritic shear. Dump samples consisted of glassy white quartz containing pyrite, galena, and chalcopyrite. The No.2 occurrence is reported (Satterly 1952) to consist of a narrow shear located at the contact between basalt and rhyolite. Quartz stringers within the shear were reported to contain less than 5% of pyrite. The No.2 occurrence consists of a narrow shear located at the contact between basalt and rhyolite. The vein is reported (Satterly 1952) to carry accessory pyrite, chalcopyrite, and galena as well as free (visible) gold. The No.4 occurrence consists of quartz stringers in rhyolite with associated traces of chalcopyrite and galena and locally as much as 20% of pyrite. Known gold mineralization which is currently (1988) believed by Perrex Resources Inc. to have economic potential is reported to be associated with shear zones oriented at azimuth 070-090. Such shears may be developed in basalt, in (silicified) rhyolite, and in the syenite plug. These mineralized shears were first recognized as a result the diamond drilling which was performed in 1986-1987. Mineralized(?) shears developed within the plug indicate that the shearing event may have been at least to some extent protracted because although some syenite hosted shears were clearly developed subsequent to the plug's solidification, others are reported to have formed prior to the magma's solidification. When hosted by basalt, an increase in fracture density and in the development of epidote and saussurite are noted proximal to shears. The silicification which affects the northern rhyolitic horizon appears to be at least in part late stage (post syenite), as syenitic dikes intrude silicified rhyolite and silicified syenite has been noted (D. Hawke, pers. comm.).
Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
---|---|---|---|---|---|---|
Iris Gold Mine | 1989 | Unclassified | 907184 | The Northern Miner, September, 25, 1989 | reserves are drill defined | Gold 2.7 g/t |
Iris Gold Mine | 1988 | Unclassified | 1088621 | MR223 | reserves are drill defined | Gold 0.6 oz/T |
File - Resident Geologist file KL-1289, KL-3170
Publication Number: Date:
Author:
Publisher Name:
Location: Kirkland Lake RGP office
Map - Gold area between lakes Abitibi and Night Hawk, District of Timiskaming
Publication Number: ARM28B Scale: 1:126,720 Date: 1998
Author: Knight C.W., Burrows A.G., Hopkins P.E., Parsons A.L.
Publisher Name: Ontario Bureau of Mines
Location:
Part - Abitibi-Night Hawk gold area, District of Timiskaming
Publication Number: ARV28-02.001 Date: 1998
Author: Knight C.W., Burrows A.G., Hopkins P.E., Parsons A.L.
Publisher Name: Ontario Bureau of Mines
Location:
Map - Township of Harker, District of Cochrane, Ontario
Publication Number: M1951-04 Date: 1997
Author: Satterly J., Hogg N.
Publisher Name: Ontario Dept. of Mines
Location:
Part - Geology of Harker Township
Publication Number: ARV60-07 Page: 35-36 Date: 1997
Author: Satterly J.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Geophysical/geochemical series, Matheson-Black River area, Harker Township, airborne electromagnetic survey, total intensity magnetic survey, District of Cochrane
Publication Number: M80599 Scale: 1:20,000 Date: 1984
Author: Questor Surveys Ltd.
Publisher Name: Ontario Geological Survey
Location:
Mono - Gold deposits of Ontario, part 1, districts of Algoma, Cochrane, Kenora, Rainy River, and Thunder Bay
Publication Number: MDC013 Page: 130 Date: 1971
Author: Ferguson S.A., Groen H.A., Haynes R.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Map - Geological series, Precambrian geology of the Magusi River area, Cochrane and Timiskaming districts
Publication Number: P2434 Scale: 1:63,360 Date: 1982
Author: Jensen L.S.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology and petrogenesis of the Archean Abitibi belt in the Kirkland Lake area, Ontario
Publication Number: MP123 Date: 1985
Author: Jensen L.S., Langford F.F.
Publisher Name: Ontario Geological Survey
Location:
Article - Kirkland Lake Resident Geologist's District - 1988
Publication Number: MP142.013 Page: 367-300 Date: 1997
Author: Meyer G., Grabowski G.P.B., Lovell H.L., Guindon D.L., Bath A.C.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological series, Quaternary geology of the Magusi River area, Cochrane and Timiskaming districts
Publication Number: P2483 Scale: 1:50,000 Date: 1982
Author: Baker C.L., Steele K.G., Seaman A.A.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian Geology of the Highway 101 Area, East of Matheson, Ontario
Publication Number: M2676 Scale: 1:50,000 Date: 2003
Author: Berger B.R., Luinstra B., Ropchan J.C.
Publisher Name: Ontario Geological Survey
Location:
Mono - Preliminary report on the Timmins-Kirkland Lake area, gold deposits file
Publication Number: OFR5467 Page: G0031 Date: 1983
Author: Hodgson C.J.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian Geology of the Ghost Range Area
Publication Number: M2563 Scale: 1:50,000 Date: 2000
Author: Berger B.R.
Publisher Name: Ontario Geological Survey
Location:
Mono - Mineral occurrences, deposits, and mines of the Black River-Matheson area
Publication Number: OFR5735 Page: 661-673 Date: 1990
Author: Bath A.C.
Publisher Name: Ontario Geological Survey
Location:
File - Res/Reg Property Visit Report #330
Publication Number: PV-330 Date: 1901
Author:
Publisher Name:
Location: Kirkland Lake RGP office
MonoMap - Geological Synthesis of the Highway 101 Area, East of Matheson, Ontario
Publication Number: OFR6091 Date: 2003
Author: Berger B.R.
Publisher Name: Ontario Geological Survey
Location:
Compend - Summary of Field Work and Other Activities, 2000
Publication Number: OFR6032 Page: 8.1-8.6 Date: 2000
Author: Ayer J.A., Baker C.L., Kelly R.I., Parker J.R., Stott G.M., Thurston P.C.
Publisher Name: Ontario Geological Survey
Location:
Compend - Summary of Field Work and Other Activities, 1999
Publication Number: OFR6000 Page: 12-1 to 12-4 Date: 1999
Author: Ayer J.A., Baker C.L., Kelly R.I., Stott G.M., Thurston P.C.
Publisher Name: Ontario Geological Survey
Location:
Publication - Canadian Mineral Deposits not Being Mined in 1989
Publication Number: MR 223 Page: ONT-100 Date: 1990
Author:
Publisher Name: Energy Mines and Resources Canada
Location: Timmins RGO
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