Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42A06NE00033

Record: MDI42A06NE00033

General

Mineral Record Identification
Record Name(s) Philadelphia Mining Syndicate - 1911, Diplomat - 1990
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 1990-Dec-31
Date Last Modified 2023-Mar-03
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Deloro

Latitude: 48° 26' 22.31"    Longitude: -81° 12' 12.69"

UTM Zone: 17    Easting: 484947.418   Northing: 5365174.108    UTM Datum: NAD83

Resident Geologist District: Timmins

NTS Grid: 42A06NE

Point Location Description: Adit located 1420 m south and 30 m W of NE corner of Deloro Township.

Location Method: Conversion from MDI

Access Description: Origianly access was gained by traveling south along Stringer's Road south of South Porcupine for about 7 km. There a gravel road (now gated) leds west about 4 km to the Deloro-Shaw Township boundary. From the point where the gravel road crosses the township boundary, an old wagon road leads north to the adit area. In 2002, the Dome Mine tailings road provides access to the area of the adit.



Exploration History

In 1911,the Philidelphia Mining Syndicate excavated a shallow adit/ramp on what was interpreted as a quartz vein. The adit is about 100 ft. long and about 35 ft. deep. The deepest 30 ft. reportedly had an average assay valy of $20 per ton. In 1963 W.H. Hansen thoroughly chip sampled the workings and received a best value of .04 (units unknown) over 5 ft. The remaining samples detected no gold. 1966 Augdome Explorations, Limited held claim under option. The option was known as the Chevalier Option. DDH 66-7 tested the iron formation under the adit and returned an assay of 0.02 opt Au over 10.8 ft. from a quartz vein, not the iron formation. (the only information for this drill hole is on a drill hole plan map) 1981, Amax Minerals Exploration conducted geological mapping and sampling of the adit. The sampling returned an average of 0.025 opt Au. 1984, John L. Kirwin for Canamax Resources Inc. mapped the geology of 2 claims, one including the adit. He noted the adit to be filled with water. 1985 Diplomat Resources Inc. slashed, stripped, washed, and examined the area around the adit. The adit itself was dewatered, and sampled and mapped in detail. 1987 J.P. Sheridan (Diepdaume Mines Ltd.) completed a magnetometer survey over an area including the adit. In 1989, Diepdaume conducted VLF and Max-Min (HLEM) surveys. In 1990, geological mapping was completed.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
T-1978, 2.4330 42A06NW8408 42A06NW8408
T-2662, 2.12925 42A06NE0430 42A06NE0430
T-2708, 2.10457 42A06NE0357 42A06NE0357
T-282, 19 42A06NE0333 42A06NE0333
T-2966, 63.4725 42A06NE0442 42A06NE0442
T-2817, 63.4117 42A06NW8492 42A06NW8492
2.15647, T-2662 42A06NE0016 42A06NE0016
2.4436, T-1978 42A06NE0417 42A06NE0417
2.7254, T-1978 42A06NE8905 42A06NE8905
25, T-1978 42A06NE8409 42A06NE8409
2.8154, T-2966 42A06NE0451 42A06NE0451

Geology

Province: Superior

Subprovince: Abitibi

Terrane: Wawa-Abitibi

Belt: Abitibi

Tectonic Assemblage: Deloro

Geological Age: Neoarchean  



Geology Comments

Dec 07, 2005 (G Seim) - The Iron formation upon which the Philidelphia Mining syndicate drove the adit occurs at the contact between mafic to intermediate metavolcanics to the south and medium- to coarse-grained felsic fragmentals to the north. A carbonate horizon occurs to the north of the felsic fragmentals. These rocks all form part of the top of the Deloro Assemblage rocks. The iron formation is described by Carson, H.D. (1967) as highly siliceous cherty iron formation.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Mafic massive flow 1 Basalt Massive Flows Footwall
Sulphide Ironstone 2 Sulphide And Oxide Facies Host
Vein 3 Quartz Host
Mafic Tuff 4 Tuff To Tuffaceous Fragmental Hanging Wall

Lithology Comments

Dec 07, 2005 (G Seim) - From Report by K.A. Jensen in T-2966: (quote)The iron formation has a shallow dip to the north of about 20 degrees. The overlying metavolcanics are slightly carbonated and consists of tuff to tuffaceous fragmentals of volcanic origin and grades into a more massive flow. The underlying volcanics appear to be slightly carbonated massive flows. The carbonatization increases near the sheared volcanics (sediment?) at the beginning of the ramp. The iron formation consists of a siliceous sulphide facies with areas extremely rich in magnetite. The most striking feature is the near verticl east-west striking fracture filling quartz stringers and veins within the iron formation. At the beginning of the ramp and about 1/2way down the ramp a wide quartz vein was exposed. It is the opinion of the author that the underlying quartz vein in the metaolcanics is the feeder vein for those in the iron formation (unquote).




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1PyriteEconomicGangue
2PyrrhotiteEconomicGangue
CarbonateAlterationCarbonatization1WeakReplacement

Mineralization Comments

Dec 07, 2005 (G Seim) - The most recent and extensive sampling of the adit was by K.A. Jensen as reported in assessment file T-2966. The best assay results reported are 0.180 opt Au over a 0.9 ft. chip sample of high sulphide (pyrite and pyrrhotite), 0.092 opt Au over a 3 ft. chip sample of pyrite-rich iron formation and 0.251 opt Au over 1.5 ft. accross a quartz vein on the floor of the ramp. All other value were less than 0.10 opt Au.



Mineral Record Details

References

File - Resident Geologist file T-271

Publication Number: Date:

Author:

Publisher Name:

Location: Timmins RGP office


Map - Timmins data series, Deloro Township, District of Thunder Bay

Publication Number: P2079 Scale: 1:15,840    Date: 1981

Author: Sangster P.J., Maharaj D.

Publisher Name: Ontario Geological Survey

Location:


MonoMap - Geology of Ogden, Deloro and Shaw townships, District of Cochrane

Publication Number: OFR5012 Page: 100  Date: 1997

Author: Carlson H.D.

Publisher Name: Ontario Dept. of Mines

Location:


Map - Deloro Township, District of Cochrane

Publication Number: P0342 Scale: 1:15,840    Date: 1997

Author: Carlson H.D.

Publisher Name: Ontario Dept. of Mines

Location:


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