Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42E03SW00040

Record: MDI42E03SW00040

General

Mineral Record Identification
Record Name(s) Dickison Lake Quartz Occurrence - 1954
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 1997-Jan-03
Date Last Modified 2022-Sep-12
Created By
Revised By

Commodities

Primary Commodities: Silica Sand



Location

Township or Area: Dickison Lake Area

Latitude: 49° 9' .19"    Longitude: -87° 25' 59.96"

UTM Zone: 16    Easting: 468401.123   Northing: 5444226.946    UTM Datum: NAD83

Resident Geologist District: Thunder Bay South

NTS Grid: 42E03SW

Point Location Description: Occurrence

Location Method: Conversion from MDI

Access Description: The occurrence is located 39 km north-northwest of the town of Schreiber. At present (1993) access to the occurrence is difficult (Figure 10) and is best achieved by helicopter. The closest road is approximately 13 km to the northeast and accesses the northern end of Dickison Lake. Another road, approximately 5 km to the northwest provides access to the western (opposite) side of the Gravel River Valley.



Exploration History

PAST: 1954 Large quartz veins were identified by M.W. Bartley as part of a regional reconnaissance survey conducted for the Canadian Pacific Railway Company. CURRENT: 1994 The quartz occurrences are all open.


Geology

Province: Superior

Subprovince: Quetico

Geological Age: Archean  



Geology Comments

Dec 07, 2005 (R Degagne) - The occurrence is located within the Quetico Subprovince and was mapped by Carter (1975). The area is underlain by a mixture of metasedimentary schists, gneisses and migmatitic rocks of Precambrian age. The occurrence located by the author is near a contact between the metasediments and migmatites. To the north is the Gravel River Fault zone. The fault is the major structural feature in the area and is marked by a 61 m (200 feet) cliff on the north side. The Gravel River and valley is within the fault zone.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Diatexite Migmatite 1 Near
Schist-Unsubdivided 2 Near
Vein 3 Qtz Host

Lithology Comments

Dec 07, 2005 (R Degagne) - The occurrence is located within the Quetico Subprovince and was mapped by Carter (1975). The area is underlain by a mixture of metasedimentary schists, gneisses and migmatitic rocks of Precambrian age. The occurrence located by the author is near a contact between the metasediments and migmatites. To the north is the Gravel River Fault zone. The fault is the major structural feature in the area and is marked by a 61 m (200 feet) cliff on the north side. The Gravel River and valley is within the fault zone.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1QuartzEconomicOre

Mineralization Comments

Dec 07, 2005 (R Degagne) - The quartz is bull white in the centre and clouded with almost completely digested host rock inclusions at the margins. CHEMICAL ANALYSIS: Analyses by Chemex Labs, Ltd. SAMPLE NO.: IM-92-038: 98.27 SiO2, 0.38 Al2O3, 0.60 Fe2O3, 0.06 MgO, 0.14 Na2O, 0.05 K2O, 0.14 CaO, <.01 MnO, 0.01 TiO2, 0.10 P205, SAMPLE NO.: IM-92-039: 98.08 SiO2, 0.35 Al2O3, 0.55 Fe2O3, 0.07 MgO, 0.14 Na2O, 0.03 K2O, 0.13 CaO, <.01 MnO, 0.01 TiO2, 0.11 P205, SAMPLE NO.: IM-92-040: 98.46 SiO2, 0.23 Al2O3, 0.40 Fe2O3, 0.02 MgO, 0.14 Na2O, 0.02 K2O, 0.13 CaO, <.01 MnO, <.01 TiO2, 0.11 P205, SAMPLE NO.: Si-metal: <.01 Al2O3, <.05 Fe2O3, <.02 CaO, <.005 TiO2. Analyses by Chemex Labs, Ltd.



Mineral Record Details

Classification
RankClassification            
1 Metamorphic
Characteristics
Rank Characteristic            
1 Vein

Mineral Zones - Size and Shape

Rank: 1       Structure Type: Contact

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Irregular

Site Visit Information

Date: Jan 03, 1997

Geologist: R Degagne

Notes: Visited in September, 1993 by P. Hinz | R. M. Landry (OGS OFR 5889, 1994) . COMMENTS/RECOMMENDATIONS: When the results are compared with specifications for silicon metal it is seen that the primary impurities (Al2O3, Fe2O3, CaO and TiO2) are all above the required tolerance levels. The results are encouraging and the author feels they warrant further investigation.



References

Map - Dickison Lake, Thunder Bay District

Publication Number: M2293 Scale: 1:63,360    Date: 1974

Author: Carter M.W.

Publisher Name: Ontario Division of Mines

Location:


Mono - Industrial Mineral Occurrences and Deposits in Northwest Ontario

Publication Number: OFR5889 Page: 64-66  Date: 1994

Author: Hinz P., Landry R.M.

Publisher Name: Ontario Geological Survey

Location:


Book - Industrial Minerals Geologist's Files, Thunder Bay

Publication Number: Date:

Author:

Publisher Name:

Location: Thunder Bay RGP


File - Schreiber-Hemlo Resident Geologist Mineral Deposit Files, Thunder Bay office

Publication Number: Min Dep Date:

Author:

Publisher Name:

Location: Thunder Bay RGP


Book - DICKISON LAKE AREA (AREA NO. 6, 1954) CPR CO., RES. GEOL. FILES, S.-H. DIST.,

Publication Number: N/A Date: 1954

Author: Bartley, M.W.

Publisher Name:

Location: Thunder Bay RGP


MonoMap - Geology of the Dickison Lake area, District of Thunder Bay

Publication Number: R123 Page: 28  Date: 1975

Author: Carter M.W.

Publisher Name: Ontario Division of Mines

Location:


Article - Northwestern Ontario Industrial Minerals Program-1991

Publication Number: MP158.008 Page: 165-180  Date: 1997

Author: Hinz P., Lucas R.T.

Publisher Name: Ontario Geological Survey

Location:


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For detailed information regarding this mineral record please contact the Thunder Bay South Resident Geologist District Office