Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42A08NW00015

Record: MDI42A08NW00015

General

Mineral Record Identification
Record Name(s) Noranda Occurrence - 1935, Temple Gold Mines Ltd. - 1945, Sherwin Mineral Ltd. - 1973, M. Charet - 1988, Northern Resources Inc. - 1996, Battle Mountain Canada - 2000
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 1991-Mar-09
Date Last Modified 2022-Sep-27
Created By
Revised By

Commodities

Primary Commodities: Gold

Secondary Commodities: Copper



Location

Township or Area: Playfair

Latitude: 48° 24' 37.7"    Longitude: -80° 24' 37.56"

UTM Zone: 17    Easting: 543629   Northing: 5362092    UTM Datum: NAD83

Resident Geologist District: Kirkland Lake

NTS Grid: 42A08NW

Point Location Description: open pit

Location Method: Based on Assessment

Access Description: Proceed west on Playfair Concession 4/5 Road From Hwy 11 and turn south on Playfair Road 3, continuing for 0.6km west of Hwy 11. Travel 3km south on road 3 and at 2.5km mark, stay right. Take the right branch at 4.8km. at 7.1km an ATV trail leads north 2-3km to site.



Exploration History

Pre-1935: Noranda Mines Ltd. - 400 feet of trenching and diamond drilled veins which could have been those of this occurrence. 1945: Temple Gold Mines Ltd.- DD-15-2506 ft; trenching, sampling. 1973-1974: Sherwin Minerals Ltd. - magnetic and geological survey; DD-2-306 m, assays 1975: Spar Holdings and Exploration Ltd. - mapping. 1988-89: M. Charet: property staked; property visited by A. C. Bath 1990: W. Weisflock and L. Salo - ground magnetometer survey; sampling completed total field mag and sampling. Best assay of 5 g/t Au.1996-2000: S. Carmichael / M. Dyment - completed 11 km of gridding, total field mag, soil geochemistry, surface stripping, washing and chip sampling.Surface sampling (grab and chip). Best assays ranged from 1.42 g/t Au to 11.56 g/t Au.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
KL-2488/ 12 42A08NW0228 42A08NW0228
KL-2488/63.3070 42A08NW0233 42A08NW0233
KL-2488/63.3154 42A08NW0227 42A08NW0227
KL-3011/2.13734 42A08NW0203 42A08NW0203
KL-3518/OP91-509 42A08NW0014 42A08NW0014
KL-4025/2.17049 42A08NW0023 42A08NW0023
KL-4270/ 2.18058 42A08NW2001 42A08NW2001
KL-4871/ 2.20777 42A08NW2011 42A08NW2011
KL-2548/2.1951 42A08NW8960 42A08NW8960
KL-2488/2.1474 42A08NW0226 42A08NW0226

Geology

Province: Superior

Subprovince: Abitibi

Terrane: Wawa-Abitibi

Belt: Abitibi

Geological Age: Archean  

Metamorphism Grade: Greenschist



Geology Comments

Apr 19, 2016 (C Salo) - Geological mapping indicates that the trenched area is underlain by weakly metamorphosed (greenschist or lower metamorphic grade) east southeast striking, steeply dipping, and south facing fine to medium grained massive, pillowed, and feldspar phyric tholeiitic basalt of the (Archean) Kinojevis Group. The occurrence is about 12.5 km southwest of the Porcupine-Destor Fault Zone and occupies part of the north limb of the east striking and east plunging Blake River Synclinorium. Intrusive rocks in the area include narrow (tens of metres in width) generally north striking diabase dikes of the (Proterozoic) Matachewan swarm and small (interpreted to be less than about 750 m in width) mafic and intermediate alkalic intrusive bodies and volumetrically minor felsic syenite (assessment files, Resident Geologist's Office, Kirkland Lake) dikes.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Mafic lava flow-unsubdivided 1 Silicified-Chloritic Basalt Near
Lamprophyre-Unsubdivided 2 Near
Granitoid-Unsubdivided 3 Felsic Dikes Near
Vein 4 Quartz-Feldspar-Chlorite-(Hematite)-Pyrite-Cp Host

Lithology Comments

Dec 07, 2005 (C Salo) - AB-88-10: Boulder chip from trench A. White quartz-calcite vein material. The sample contains parallel seams of chlorite and pyrite which give the vein a sheeted appearance. Silicified mafic xenoliths within the vein contain abundant less than 1 mm size pyrite cubes. Large (2-4 mm wide) pyrite cubes are also present in the vein. This sample contains 3-5% of pyrite. AB-88-11: Boulder chip of pyritic basalt marginal to the vein sampled by sample AB-88-10. 1 mm grained diabasic basalt or diabase containing 5-7% of 1 mm grained subidioblastic pyrite cubes. The pyrite is associated with variably developed silicification as quartz lenses, quartz-feldspar veinlets, and irregular zones of pervasively silicified mafic material. The sample is not sheared and does not contain carbonate minerals. AB-88-16: Muck grab from the bottom of trench B. Well mineralized sample consisting of sheeted white quartz vein material hosted by varicolored pervasively altered host rock. Vein material is composed of white quartz with numerous parallel seams which give the vein a sheeted appearance. Some of the seams are mauve colored, probably due to hematite. The material hosting the veins is light grey to mauve colored, pervasively silicified, nonmagnetic, and contains 7-10% of subidioblastic disseminated 1-2 mm size pyrite cubes, traces chalcopyrite, and 5-7% of irregular flecks of leucoxene. No carbonate minerals are present. AB-88-17: Chip from trench C. 8 cm wide quartz-chlorite vein material similar to previous samples. Note that one vein wall is sharp, with a narrow (1-2 cm wide) zone of pervasive silicification while the other wall is irregular with a larger (at least 8 cm wide) zone of pervasive silicification. The altered host rock marginal to the vein is light grey, nonmagnetic, pervasively silicified, and leucoxenitic. Pyrite is confined to the altered host rock marginal to the vein and constitutes less than 2% of the sample.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1PyriteEconomicGangue
2ChalcopyriteEconomicGangue
3HematiteEconomicGangue
4ChloriteEconomicGangue
5QuartzEconomicGangue
SilicaAlterationSilicification1UnknownReplacement
ChloriteAlterationChloritic2UnknownReplacement

Mineralization Comments

Apr 19, 2016 (A Wilson) - Sherwin Minerals Ltd. DDH B returned assays of trace Au and 0.08% Cu over 0.5 ft. Trench chip samples taken by Temple Gold Mines returned gold tenors as high as 0.22 ounce of gold per ton across 21 feet. The best assay from the Weisflock sampling returned an assay of 5186 ppb Au.


Apr 19, 2016 (C Salo) - Trench A is oriented at az. 115, is about 25 m long, 2-3 m wide, 1.5-2.0 m deep. Spotty fine-grained to medium-grained py occurs with occasional greater py contents, locally as much as 15%. It is likely that these are partly buried boulders. A 5' long (chip?) sample from the east part of this trench is reported by Temple (ass. files) to have assayed 0.36 oz./t Au. Averaging 0.156, 0.188, and 0.062 oz./t Aurespectively, and background levels of Ag, Cu, Pb, and Zn. Trench B is orientated. at az. 095, is about 15 m long, 2m wide, and 2-3 m deep. The Temple assessment. file indicated that (chip?) samples from this trench which were obtained prior to 1946 aver. 0.06 oz./ton Au across 16' within and marginal to the quartz vein. Samples averaged 0.055, 0.003, 0.045, 0.002 & 0.232 oz./t Au resp. with background levels of Ag, Cu, Pb, and Zn. Trench C is orientated at az. 120, is about 13 m long, about 1.5 m deep, and 1.5-2.0 m wide. Veins contain py at trench B. (Chip?) sampling from this trench prior to 1946 are reported by Temple to be anomalous gold content 0.01 oz. Au/ton along much of the trench's length, with 6' averaging 0.04 oz./t Au and 6' averaging 0.06 oz./t Au at the west and east ends resp. Samples assayed 0.038, 0.036, and 0.112 oz./t Au respectively with background levels of Ag, Cu, Pb, and Zn. Trench D is orientated at az. 095, is about 15 m long, 2m wide, and 1.5-2.5 m deep. (Chip?) sampling completed prior to 1946 indicated (Temple ass. file) that this trench aver. 0.15 oz./t Au over a 24' sample length. Sample assayed 0.431 oz./t Au ,0.025 oz. Ag/ ton, and background levels of base metals.Trench E is orientated at az. 106, is 10 m long, 2-3 m wide, 0-2 m deep. (Chip?) samples taken along the trench prior to 1946 indicate that the trench at one time exposed Au min. aver. 0.17 oz. Au/ton across a 27' sampling interval, including 0.22 oz./t Au across 21' (Temple ass. file). Trench F is orientated at az. 106, is 12 m long, 2-3 m wide, 2-3 m deep and was badly overgrown.



Mineral Record Details

Classification
RankClassification            
1 Vein
Characteristics
Rank Characteristic            
1 Vein

References

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Location:


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For detailed information regarding this mineral record please contact the Kirkland Lake Resident Geologist District Office