Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI41O10NW00008

Record: MDI41O10NW00008

General

Mineral Record Identification
Record Name(s) North Greenlaw Iron Formation - 1968
Related Record Type Simple
Related Record(s)
Record Status Discretionary Occurrence
Date Created 1994-May-30
Date Last Modified 2022-Sep-27
Created By
Revised By

Commodities

Primary Commodities: Iron

Secondary Commodities: Gold



Location

Township or Area: Greenlaw

Latitude: 47° 43' 57.61"    Longitude: -82° 47' 35.4"

UTM Zone: 17    Easting: 365550.21   Northing: 5288145.44    UTM Datum: NAD83

Resident Geologist District: Timmins

NTS Grid: 41O10NW

Point Location Description: Outcrop of iron formation along north shore of Ridout Lake.

Location Method: Field Visit with GPS

Access Description: Access is by way of Highway 667, south of Chapleau, between Highway 129 and the town of Sultan. Take the Kormak Rd. north past the Canadian National Railway line. A logging road leads north then east into Greenlaw Twp. The area north of Ridout lake is accessible by ATV along a small trail that follows the north shore of Ridout Lake.



Exploration History

1980-81: Granges Exploration Ltd. drilled 7 holes in an area to the west of Ridout Lake for a total of 504 m. All but two of these holes intersected iron formation. Other rock types include intermediate to felsic volcanics. 1983: Noranda Exploration drilled two holes into iron formation to the west of Ridout Lake. The combined length of the drill holes was 469 m. Anomalous metal values as high as 0.011 oz./t Au and 1.16% Zn were reported in core assays. 1984: Noranda Exploration conducted a magnetic and electromagnetic survey over claims along the north shore extending to the west and the south shore of Ridout Lake. Noranda also conducted a geological mapping and geochemical humus survey over an area that include Ridout Lake and Little Ridout Lake to the east of the iron formation exposure. Humus sample were analyzed for Au but only discontinuous single anomalies were uncovered. Aerodat Limited flew a combined helicopter borne magnetic, electromagnetic and VLF survey for Kelly Kerr (John Larche Property) over the west end of Ridout Lake which included the showing. 1985: Granges Exploration Ltd. conducted a soil geochemical survey due west of Ridout Lake over a block of 11 claims. No interesting anomalies were discovered and further work was not recommended. 1993: Cameco Corporation carried out a geological mapping and VLF electromagnetic survey over the area in the search for gold. No significant gold values were obtained in this program.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
T-2823 / 2.7262 41O10NW0015 41O10NW0015
T-2854 / 2.9170 41O10NE0019 41O10NE0019
T-3641 / 2.16301 41O10NW0006 41O10NW0006
T-3641 / 2.15494 41O10NW0012 41O10NW0012
T-2823 41O10NW9064 41O10NW9064
T-2854 / 2.6951 41O10NE0024 41O10NE0024

Geology

Province: Superior

Subprovince: Abitibi

Terrane: Wawa-Abitibi

Belt: Swayze

Tectonic Assemblage: Ridout

Geological Age: Neoarchean   Geochronological Age: 2730+/- 3 MA   Geochron. Age Ref.: OF 3384E

Metamorphism Type: Regional

Metamorphism Grade: Greenschist



Geology Comments

Dec 07, 2005 (K Houle) - Iron formation is highly sheared and schistose which has removed any obvious stratification. The contact between the iron formation and the surrounding rock is described as gradational. The schistosity has been measured as striking east-west and dipping steeply to the north.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Carbonate Ironstone 1 Carbonate Facies? Banded Iron Formation Host
Intermediate lava flow-unsubdivided 2 Andesite Adjacent

Lithology Comments

Dec 07, 2005 (K Houle) - The iron formation along the north shore of Ridout Lake is described as being folded, sheared, brecciated and closely associated with schistose intermediate to felsic volcanics. The iron formation is said to be cross cut by numerous small irregular quartz veins and the most common minerals present are quartz, calcite, siderite, limonite, pyrite and epidote.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1PyriteEconomicOre
2HematiteEconomicOre
3LimoniteEconomicOre
LimoniteAlterationUnknown1StrongReplacement

Mineralization Comments

Dec 07, 2005 (K Houle) - It has been mentioned that quartz calcite, siderite, limonite, pyrite and epidote are common constituents of the iron formation (Donovan, 1968).


Jul 25, 2013 (A Wilson) - Grab samples taken by the OGS in 1994 returned an assay of 0.01 g/t Au and 0.1 g/t Ag from a sample of the iron formation.



Assay Samples

Assay Samples
CommodityAnalytical MethodDigestion Method ResultUnitLimitQualifier
CopperUnknown.0025%
GoldUnknown.01ppm
LeadUnknown.0001%
MolybdenumUnknown.0001%
NickelUnknown.0014%
SilverUnknown.1ppm
ZincUnknown.0018%

Mineral Record Details

Classification
RankClassification            
1 Sedimentary
Characteristics
Rank Characteristic            
1 Sheared

Mineral Zones - Size and Shape

Rank: 1       Structure Type: Shear

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Unknown 1600 120 270 70 N/A N/A

Site Visit Information

Date: Jun 18, 1994

Geologist: K Houle

Notes: Iron formation sequence to the north of Ridout Lake just south of an ATV trail was visited. What at first glance appeared to be a ridge of outcrop consisted mainly of float and boulders. Outcrop was located at the bottom of the ridge on the lake side and consisted of interbedded silicified sediments and interbedded chert. Unit at this location was found to be highly sheared and schistose with cross cutting bands of dark brown material 1-2 cm. in width. Unit is also cut by irregular white quartz and trace to 2% fine pyrite was observed at this location.



References

Map - Tooms and Greenlaw townships, Sudbury District

Publication Number: M2121 Scale: 1:31,680    Date: 1997

Author: Donovan J.F.

Publisher Name: Ontario Dept. of Mines

Location:


Publication - Preliminary report on Woman river and ridout map areas, Sudbury district, Ontario; Geological Survey of Canada, Memoir 157

Publication Number: GSC Mem 157 Page: 24-25  Date: 1929

Author: Emmons, R.C. and Thomson, E.

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/100840


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: 41O-79  Date: 1985

Author: Rose, D. G.

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/129999


Map - Geology, Swayze greenstone belt, Sultan, Ontario

Publication Number: OF 3384E Scale: 1:50,000    Date: 1999

Author: Heather, K B; Shore, G T

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/210453


Part - Geology of the Swayze gold area

Publication Number: ARV43-03.001 Page: 11-13  Date: 1998

Author: Rickaby H.C.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Geology of Halcrow-Ridout lakes area, District of Sudbury

Publication Number: R063 Page: 17-19, 34  Date: 1968

Author: Donovan J.F.

Publisher Name: Ontario Dept. of Mines

Location:


File - Resident Geologist files 1980, air photos

Publication Number: Date: 1996

Author:

Publisher Name:

Location:


Mono - Iron deposits of Ontario

Publication Number: MDC011 Page: 336  Date: 1968

Author: Shklanka R.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Mineral Prospects of the Swayze Greenstone Belt (Volume 1, Parts of NTS 41 O and Volume 2, Parts of NTS 41 P, 42 A and 42 B)

Publication Number: OFR5912 Page: 141-143  Date: 1995

Author: Fumerton S.L., Houle K.A.

Publisher Name: Ontario Geological Survey

Location:


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