Ontario Geological Survey
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MDI42E10NW00024
| Record Name(s) | Burroughs Syndicate Central - 1938 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 1991-Feb-05 |
| Date Last Modified | 2022-Sep-27 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: Coltham
Latitude: 49° 39' 23.59" Longitude: -86° 44' 55.66"
UTM Zone: 16 Easting: 518131.121 Northing: 5500476.147 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 42E10NE, 42E10NW
Point Location Description: Trenches and diamond-drill holes.
Location Method: Data Compilation
Access Description: The property is located in north central Coltham Township. The property can be reached by travelling the Trans Canada Highway 11 for 9.5 km east of the turn-off to Geraldton (Hwy 584) and south and east on Eldee Lake Road for about 4.8 km, to the east-west baseline which crosses the property. The occurrence is located approximately 4.0 km east along the baseline and 300 m to the south.
1938: The claims covering the occurrence were staked by Rob Hobs (TB 26256 and TB 27050). Surface exploration was performed. 1939: Claims transferred to J.E. Burroughs of the Burroughs Syndicate and later optioned to J.E. Greenburgh. Mag and geological surveys were conducted, followed by trenching and diamond-drilling. Surface channel sampling and ten holes were drilled to test the occurrence. 1941: Claims surveyed and further surface work performed. 1944: J.E. Greenburgh patented the claims. 1945: Patents revoked. 1983: Property restaked by Michael Malouf of Quarternary Mining and Exploration Company Ltd. 1984: A grid was cut on which magnetometer and EM surveys were conducted. Geraldton Longlac Gold Inc. was formed by M. Malouf and all claims covering the Burroughs occurrences were transferred to this new company. 1987: Geraldton Longlac Gold Inc. conducted an extensive overburden stripping program, primarily in an area between Burroughs Central and Burroughs East occurrences (claim TB 677042). Diamond drilling was also undertaken. 1994: Geraldton Longlac sold the property to Hardrock Extension Inc. 1994-95: Hardrock Extension carried out power stripping and sampling. 1999: Hardrock Extension drilled 2 DDH. 2016: Hardrock Extension carried out power stripping and sampling.
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| 12 | 42E10NE0066 | 42E10NE0066 |
| 63.5345 | 42E10NE0061 | 42E10NE0061 |
| 2.7267 | 42E10NE0068 | 42E10NE0068 |
| 2.58328 | 20000015348 | 20000015348 |
| 63.5159 | 42E10NE0063 | 42E10NE0063 |
Province: Superior
Subprovince: Wabigoon
Terrane: Eastern Wabigoon
Belt: Beardmore-Geraldton
Geological Age: Archean
Dec 07, 2005 (G White) - The Burroughs Syndicate occurrence (West) is located in the southeastern portion of the main Beardmore-Geraldton metasedimentary-metavolcanic belt. The Croll Lake stock is situated immediately north of the occurrence and is postulated to be the heat source for much of the gold mineralization in the Geraldton camp. The three Burroughs occurrences (West, Central, and East) lie within the eastern portion of what is termed the 'Barton Bay Deformation Zone' (Macdonald 1983). This is a lithotectonic package which is up to 5 km wide, is associated with the Bankfield-Tombill fault in the Geraldton area (Lavigne 1983, Buck and Williams 1984). The deformation zone is defined by anastomosing shear zones with intervening areas of less deformed rocks. Just east of the Burroughs occurrences, the Barton Bay Deformation Zone is well exposed along the west shore of Long Lake where simple shear strain indicators are found over a 2 km width. This deformation zone continues east of Long Lake and studies indicate that it may be up to 4 km wide along the east shore.
Dec 07, 2005 (B Nelson) - The property is underlain by Timiskaming sediments and basic to intermediate metavolcanic units wrapped around the southern flank of a large granite pluton. The Keewatin volcanic rocks in the southern belt consist mainly of chloritic tuffs and breccias. They appear to be related to the units found southeast of the MacLeod -Cockshutt and Hard Rock Mines and lie stratigraphically above the massive andesite and basalt flow rocks. Shearing and metamorphism obliterate much of the primary pillow structures. Mineral assemblages are high in amphibole, chlorite, epidote, carbonate and biotite. The iron formation marks the north limb of a major syncline, but Archibald (1983) believes the units described above form part of the southern limit of an overturned synclinal structure. He also believes that the property lies along the extension of the Bankfield-Tombill strike fault which is expressed as shearing in the units found on the property. To the east, quartz porphyry intrusions are intercalated with iron formations and conglomerates. The gold occurs in fissures or irregular quartz-filled openings in greywacke and iron formation. Gold occurs where the vein openings intersect iron bands. Sulphides occur in a matrix of quartz broken iron formation, chlorite or a combination of these. The best combination is believed to be coarse sulphides in quartz. Where the veins pass into greywacke, the sulphides disappear.
| Rock Type | Rank | Composition | Texture | Relationship | Sandstone | 1 | Greywacke | Tuffaceous | Host |
|---|---|---|---|---|
| Ironstone-unsubdivided | 2 | Host | ||
| Vein | 3 | Quartz-Chlorite | Host | |
| Granite | 4 | Near | ||
| Breccia-unsubdivided | 5 | Sheared | Near | |
| Mafic lava flow-unsubdivided | 6 | Near |
Dec 07, 2005 (B Nelson) - Tuffs, agglomerates and lenses of greywacke are found interflowed with the volcanic sequences. These units generally strike east-west and dip steeply to the south. The volcanics lie disconformably below the sediments which also strike east-west and dip 75 degrees south.
| 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 | Specularite | Economic | Ore | ||||
| 1 | Quartz | Economic | Gangue | ||||
| Quartz | Alteration | Silicification | 1 |
Dec 07, 2005 (B Nelson) - The following are some assay values that came from the work of J.E. Greenburgh in 1939: Channel sample #6 (0.46 m wide) assayed 0.34 oz/ton Au. Channel sample #12 (0.51 m wide) assayed 1.08 oz/ton Au. The check assay ran 1.53 oz/ton Au. Channel sample #26 (0.40 m wide) assayed 0.55 oz/ton Au. Channel sample #60 (.12 m total) assayed 0.45 oz/ton Au. X-ray diamond-drill hole 6 provided an assay that ran 0.34 oz/ton Au over 0.40 m. X-ray diamond-drill hole 7 provided an assay that ran 0.36 oz/ton Au over 0.30 m.
File - Resident Geologist files AFRO 1939-40, Coltham Township
Publication Number: Date: 1939
Author:
Publisher Name:
Location: Thunder Bay RGP Assessment Files
Map - Long Lake-Pagwachuan Lake area, District of Thunder Bay, Ontario
Publication Number: ARM46B Scale: 1:63,360 Date: 1997
Author: Fairbairn H.W., Macdonald R.D.
Publisher Name: Ontario Dept. of Mines
Location:
File - Northern Miner historical file
Publication Number: NMiner Date:
Author:
Publisher Name:
Location: Thunder Bay RGP
Map - Kenogamisis River area, District of Thunder Bay, Ontario
Publication Number: ARM49M Scale: 1:63,360 Date: 1997
Author: Macdonald R.D.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Compilation series, Geraldton sheet, Thunder Bay and Cochrane districts
Publication Number: P0241 Scale: 1:126,720 Date: 1984
Author: Stott G.M., McConnell C.D., Mason J.K.
Publisher Name: Ontario Geological Survey
Location:
Part - Geology of the Kenogamisis River area
Publication Number: ARV49-07.002 Date: 1998
Author: Macdonald R.D.
Publisher Name: Ontario Dept. of Mines
Location:
Folio - McBean Lake area, District of Thunder Bay
Publication Number: GDIF047 Date: 1997
Author: Thunder Bay RGO
Publisher Name: Ontario Geological Survey
Location: Thunder Bay RGP
Map - Mineral deposits series, Ontario mineral potential, Longlac sheet, districts of Thunder Bay and Cochrane
Publication Number: P1527 Scale: 1:250,000 Date: 1978
Author: Springer J.S.
Publisher Name: Ontario Geological Survey
Location:
Map - Tashota-Geraldton sheet, geological compilation series, Thunder Bay and Cochrane districts
Publication Number: M2102 Date: 1997
Author: Pye E.G., Harris F.R., Fenwick K.G., Baillie J.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Gold occurrences, prospects, and deposits of the Beardmore-Geraldton area, districts of Thunder Bay and Cochrane
Publication Number: OFR5630 Date: 1986
Author: Mason J.K., White G.D.
Publisher Name: Ontario Geological Survey
Location:
File - Resident Geologist mineral deposit files
Publication Number: Min Dep Date:
Author:
Publisher Name:
Location: Thunder Bay RGP
Map - Precambrian geology, northern Long Lake area, southern part
Publication Number: M2539 Scale: 1:20,000 Date: 1991
Author: Kresz D.U., Zayachivsky B., Oiye S.H.
Publisher Name: Ontario Geological Survey
Location:
Part - Geology of the northern Long Lake area
Publication Number: ARV46-03.001 Date: 1997
Author: Fairbairn H.W.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Precambrian geology, Northern Long Lake area
Publication Number: R273 Date: 1991
Author: Kresz D.U., Zayachivsky B.
Publisher Name: Ontario Geological Survey
Location:
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