Ontario Geological Survey
Permanent Link to this Record:
MDI31F03NW00044
Record Name(s) | Simon Copper Property - 1956, Harvey Simon Property - 1964, Simon Deposit - 1980, Simon Property South Showing - 1960 |
---|---|
Related Record Type | Compound |
Related Record(s) | |
Record Status | Developed Prospect With Reported Reserves or Resources |
Date Created | 1981-Mar-20 |
Date Last Modified | 2024-Jan-31 |
Created By | |
Revised By |
Primary Commodities: Copper, Zinc
Township or Area: Lyndoch
Latitude: 45° 12' 29.05" Longitude: -77° 18' 47.92"
UTM Zone: 18 Easting: 318337 Northing: 5008668 UTM Datum: NAD83
Resident Geologist District: Southern Ontario
NTS Grid: 31F03NW
Point Location Description: outcrop
Location Method: Field Visit with GPS
Access Description: The deposit is located about 8 km N of Denbigh, 3.2 km NW of Slate Falls, on the E slope of a large hill. Access is via a dirt road which passes within 900 m of the deposit. Drive NW along the Slate Falls Road from Hwy 41 until it ends, a distance of 5.2 km. From this point take a dirt lumber road (on the right) N for about 2 km to the opposite side of the sandy hill. From this point the deposit is reached on foot, 920 m at 250 degrees. The S showing lies near the S boundary of the E half of lot 1, Range B, Lyndoch. The 2 groups of workings are 300 m apart in a N-S direction, connected by an overgrown dirt road. Both main showings are in Lyndoch township but some work was carried out in Denbigh.
1961 : Noranda Explorations Ltd optioned the Harvey Simon property (South showing), carried out geophysics and mapping and drilled 13 holes (2,502 ft) in total on claims in lot 1, Range B, Lyndoch and lot 40, East Range, Denbigh 1965 : Young-Davidson Mines Ltd carried out geophysics and drilled 7 holes ( 3,807 ft). 1992: Noranda Explorations Ltd also carried out exploration on adjoining lots 16-20 in con 1 and 2, Lyndoch, and lots 16-20 in con 15 and 16, Denbigh, where they drilled 2 holes (406 m), geochemistry. 2000: Pelangio Mines Ltd. diamond drilled 3 holes for a total of 486 m to test the down plunge extension of the South Zone Deposit and evaluate copper and zinc mineralization at depth. 2003: Pelangio Mines Inc. had airborne EM and Mag surveys completed over the property. 2004: They continued with a ground EM survey on a cut grid. Diamond drilling was performed on concession I, lots 17-21. Five holes totalling 1008m was completed. Two holes were targeted to evaluate new anomalies and 3 holes were located in the main zone (press release Pelangio Mines Inc., January 17, 2005). 2006, 2007: Adroit Resources Inc. acquired the property in 2006 and performed linecutting, ground EM and Mag then at the start of 2007 completed 20 diamond drill holes for a total of 3,029m.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
Tweed files Lyndoch #42, Denbigh #6 / 2.20984 | 31F03NW2004 | 31F03NW2004 |
Tweed files Lyndoch #43, Denbigh #7 / 2.26993 | 31F03NW2007 | 31F03NW2007 |
Tweed files Lyndoch #44, Denbigh #8 / 2.28816 | 31F03NW2009 | 31F03NW2009 |
Tweed files, Lyndoch #45, Denbigh #9 / 2.30860 | 20000000896 | 20000000896 |
Tweed files, Lyndoch #46, Denbigh #10 / 2.36127 | 20000002442 | 20000002442 |
Tweed files Lyndoch #47, Denbigh #11 / 2.36127 | 20000002442 | 20000002442 |
OP92-489 | 31F03NW0005 | 31F03NW0005 |
15 / 10 | 31F03NW9426 | 31F03NW9426 |
10 | 31F03NW9427 | 31F03NW9427 |
Province: Grenville
Subprovince: Central Metasedimentary Belt
Geological Age: Mesoproterozoic
Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 | Amphibolitic | Host |
---|---|---|---|---|
Pegmatite | 2 | Granite | Intrudes |
Apr 29, 2019 (C Papertzian) - The main deposit (S showing - near the S boundary of the E half of lot 1, Range B) consists of disseminated cp, po and minor py and sp in a conformable lens 3 m thick, 180 m long and continuous to a depth of at least 107 m as proven by drilling. It is hosted by amphibolite paragneiss. The lens is reported to contain a total of 253,000 tons of 1.09 % Cu. The N showing (about 300 m N of the S showing) consists of minor cp disseminated within a small lens of massive magnetite. It is hosted in metagabbro, about 2 ft thick and pinches out within 15 ft along strike. There is a small showing of massive py and cp in a zone about 1 ft wide, at a point 500 ft E of the N showing. Another small showing, of coarse, disseminated py and cp in amphibolite, is located on the road between the 2 main showings. The S deposit is considered to be very similar to the New Calumet Zn-Pb-Ag mine on Calumet Island in the Ottawa River. See MDC 20 (1980) for a good description and map.
Jul 15, 2011 (A Wilson) - The main rock type is a fine- to medium-grained amphibolite gneiss composed of hornblende and plagioclase with minor biotite and quartz. In places accessory garnet is abundant. The foliation strikes N to N15°E and dips 30-50° E with local dips of 65-75° E. Coarse-grained leucogranite in various amounts as injections and dikes.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Chalcopyrite | Economic | Ore | ||||
2 | Pyrite | Economic | Ore | ||||
3 | Sphalerite | Economic | Ore | ||||
4 | Specularite | Economic | Ore | ||||
5 | Garnet | Economic | Ore | ||||
6 | Magnetite | Economic | Ore | ||||
7 | Pyrrhotite | Economic | Ore |
Jul 15, 2011 (A Wilson) - Assays from the 1961 diamond drilling program completed by Noranda returned assays ranging from 0.21% Cu over 23.2 feet in DDH 1 to 2.48% Cu over 9.54 ft in DDH 11. The main (south) property consists of disseminated chalcopyrite, pyrrhotite and minor pyrite and sphalerite in a conformable lens 3 m thick, 180 m long and continuous to a depth of at least 107 m. The northern showing consists of minor chalcopyrite disseminated within a small lens of massive magnetite. Grab samples collected from the northern trenches returned Cu values between 0.16 and 0.35% Cu and 0.04 to 3.4% Zn
Rank | Characteristic |
---|---|
1 | Disseminated |
Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
---|---|---|---|---|---|---|
Simon Copper South Showing | 1962 | Unclassified | 229518 | MDC020 p. 45 | The South Zone contains 253,000 tons of 1.09% Cu to a depth of 350 feet | Copper 1.09 % |
File - Tweed file Lyndoch #1, 2
Publication Number: Date:
Author:
Publisher Name:
Location: Tweed RGP office
Part - Geology of the Brudenell-Raglan area
Publication Number: ARV62-05 Page: 71 Date: 1998
Author: Hewitt D.F., Carlson H.D.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of Ashby and Denbigh townships
Publication Number: R026 Page: 35-36 Date: 1997
Author: Evans A.M.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Iron deposits of Ontario
Publication Number: MDC011 Page: 322 Date: 1968
Author: Shklanka R.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Copper, nickel, lead and zinc deposits of Ontario
Publication Number: MDC012 Page: 226-227 Date: 1969
Author: Shklanka R.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of base metal, precious metal, iron, and molybdenum deposits in the Pembroke-Renfrew area
Publication Number: MDC020 Page: 45-48 Date: 1980
Author: Carter T.R., Colvine A.C., Meyn H.D.
Publisher Name: Ontario Geological Survey
Location:
Mono - Metallogeny of the Grenville Province, southeastern Ontario
Publication Number: OFR5515 Page: 30, 206-215 Date: 1984
Author: Carter T.R.
Publisher Name: Ontario Geological Survey
Location:
Map - Brudenell-Raglan area, County of Renfrew, Ontario
Publication Number: M1953-02 Scale: 1:63,360 Date: 1997
Author: Hewitt D.F.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Precambrian Geology, Denbigh Area
Publication Number: P3437 Scale: 1:50,000 Date: 2001
Author: Lumbers S.B., Vertolli V.M.
Publisher Name: Ontario Geological Survey
Location:
We are continuously updating our assessment file / technical report information. If you notice errors in the data, please contact us.
Please review our Terms of Use agreement for this data product.
For detailed information regarding this mineral record please contact the Southern Ontario Resident Geologist District Office