Ontario Geological Survey
Permanent Link to this Record:
MDI000000001999
Record Name(s) | I Zone - 1986, Dyke 10 - 1987 |
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Related Record(s) | |
Record Status | Prospect |
Date Created | 2016-Aug-18 |
Date Last Modified | 2023-Feb-03 |
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Revised By |
Primary Commodities: Gold
Township or Area: Duckworth
Latitude: 48° 33' 31.59" Longitude: -90° 5' 23.54"
UTM Zone: 15 Easting: 714716.5 Northing: 5382498 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 52B09SE
Point Location Description: Sample A685565 in I Zone trench from Assessment report 20000019257
Location Method: Based on Assessment
Access Description: The prospect is easily accessible through an all-weather gravel road, the Duckworth road, which branches from the paved road leading to the former Inco Shebandowan Mine, some 2 kilometers from Highway 11.
1896: In the Goldcreek area, gold was first reported by government geologist on the shores of Gold Creek. 1943-44: Gunflint Iron Mines Ltd. completed a surface work program of prospecting, channel sampling and 2,796 feet (852 m) of diamond drilling (12 holes) to test the Matawin iron formation, it was found that some gold mineralization was found in the general area of the I-Zone. 1956-57: Monpre Mining Company Ltd. explored a block of claims along the Matawin iron formation in central Duckworth and Laurie townships. Ground geophysics, geological mapping and 10,592 feet (3,228 m) of diamond drilling delineated 100 million tons of 30% Fe and an open pit mining pre-feasibility plan was prepared (Litchtblau 1997 and OGS 1995). The property went dormant until 1983 when the patented claims lapsed. 1983-84: Jalna Resources Ltd completed a significant exploration over a large area of Duckworth and Laurie Townships including ground and airborne surveys, geological mapping, geochemical surveys, trenching, sampling and overburden drilling. Prospecting verified earlier anomalous gold showings in the area of the I Zone. 1984-85: Anaconda Canada Exploration Ltd. (“Anaconda”) followed up the work completed by Jalna with 3,665 feet (1117 m) of diamond drilling, in 13 holes and confirmed the anomalous gold values over the I-Zone. 1987: INCO Gold completed a geological and magnetometer survey over a large portion of Duckworth and Laurie Townships identifying fifteen areas of anomalous gold mineralization and/or strong alteration. The I Zone was target "I". 1988: Stripping and trenching was undertaken. 1989: A 1 km gravel road was constructed to the I-Zone. Further stripping and trenching, detailed mapping and detailed channel sampling (238 samples) over 150 linear feet (46 m) on the I–Zone and other parts of the syenite. A 1273 m of diamond drilling program consisting of 11 holes were carried out on the I-zone. A bulk cyanide test from the channel samples collected on the I-Zone and leached with cyanide over a 110 hour period demonstrating a recovery of 96.2% with an average grade of 1.05 g/t Au. 1995-97 Landore Resources Inc. carried out ground and airborne geophysics, mapping, stripping, channel sampling and a seven diamond drill hole program totalling 304.8 m. A cyanide leach of pulp from drill core returned an average of 6,75 g/t Au for a recovery of 92% confirming the leach test conducted by Inco in 1989. 2003: Landore completed a small mapping and prospecting program. 2006 HELM Resources Inc. completed a 498 line km airborne VTEM and total field magnetic survey over the Property. Scodnick and Allard completed a Beep Mat Survey over the I-Zone. 2007: Mengold Resources Inc. optioned the property and did reconnaissance geology, stripping and channel sampling in the South and the I Zones. Abitibi Geophysique completed 92.1 line-km of magnetometric (“Mag”); 75.1 line-km of Horizontal Loop Electromagnetic (“HLEM”) also referred to as MaxMin; and 22.8 line-km of Induced Polarization (“IP”) for Mengold. 2008: A stripping was done over Dyke #1 on the I Zone to extend the area already uncovered by Inco in the 1980s. 2020: Portofino Resources Inc. carried out prospecting and sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.17721 | 52B09SE0093 | 52B09SE0093 |
2.36379 | 20000002517 | 20000002517 |
2.10955 | 52B09SE0032 | 52B09SE0032 |
2.35050 | 20000002677 | 20000002677 |
2.40426 | 20000003869 | 20000003869 |
2.39442 | 20000003511 | 20000003511 |
3880, 3881 | 20000019257 | 20000019257 |
22 | 52B09SE0016 | 52B09SE0016 |
2.18110 | 52A12SW2006 | 52A12SW2006 |
18 | 52B09SE0037 | 52B09SE0037 |
2.16790 | 52B09SE0041 | 52B09SE0041 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Shebandowan
Geological Age: Archean
Aug 19, 2016 (Andrew Tims) - The I-Zone has a syenite to quartz-syenite dyke trending 070º with widths of 1.0 m to 5.0 m orange-grey, fine to medium grain, massive, equigranular, feldspar rich, with less than 1% disseminated pyrite. The syenite contacts with the argillaceous rhythmically banded iron formation are sharp and there may be some BIF xenoliths in the dykes as well having the dykes split. The syenites are well fractured and penetrated bynorth-northwest trending quartz-veins that generally have more pyrite (2% to 5%) adjacent to the veins.
Rock Type | Rank | Composition | Texture | Relationship | Syenite | 1 | Host |
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Ironstone-unsubdivided | 2 | Pyritic argillite and chert of BIF | Adjacent |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore |
Aug 23, 2016 (Andrew Tims) - Two samples were collected from the I-Zone (dyke 10) within a syenitic dyke with a 5 cm wide quartz vein (5 cm) mineralized with 3% to 5% pyrite yeilding and assay of 6.46 g/t Au. Diamond drill hole 95-04 intersected 3.92 g/t Au over 41 m. JF Scott Field Visit: NAD27 15U 715112/5382523 Inco Dike 10 @ 18.7 g/ Au; NAD27 15U 714739/5382444 Inco X Zone Dike 26 @ 20.9 g/t Au; NAD27 15U 714701/5382498 Inco I-zone Qtz ladder veins in a syenitic dike intruding Temiskaming-type metaseds. Dyke 10 (I-Zone) was tested in 1987 and the hole DDH-74874 intersected a syenite dyke cut by quartz veining with traces of pyrite at 141.47 m assaying 1.98 ppm Au over 0.87 m. A second hole DDH-74875 intersected a syenite dyke with a pyrite band at 137.78 m assaying 2.47 ppm Au over 0.43 m and a third hole DDH-74876 intersected a syenite dyke cut by quartz veins with visible gold and traces of pyrite and chalcopyrite at 69.19 m assaying 3.28 ppm Au over 5.64 m. 2008: at the exposed western end of the syenite dyke the company produced a mini-bulk sample of approximately 1000 kg that returned an average gold grade of 9.9 g/t. Some selected samples throughout the dyke returned gold values between 22.3 and 234.0 g/t.
Jan 31, 2023 (Therese Pettigrew) - Sample A685565 collected in 2020 returned 45.6 g/t Au from a weakly silicified syenite with a 1 cm wide quartz vein and 1% pyrite (Assessment report 20000019257).
Map - Precambrian Geology, Duckworth Township
Publication Number: M2621 Scale: 1:20,000 Date: 1995
Author: Rogers M.C.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological series, Precambrian geology, Laurie Township, District of Thunder Bay
Publication Number: P3083 Scale: 1:15,840 Date: 1987
Author: Carter M.W.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Precambrian Geology, Adrian, Marks, Sackville, Aldina and Duckworth Townships
Publication Number: R295 Date: 1995
Author: Rogers M.C., Berger B.R.
Publisher Name: Ontario Geological Survey
Location:
Mono - Geology of Adrian, Marks, Sackville, Aldina and Duckworth Townships, District of Thunder Bay
Publication Number: OFR5896 Date: 1994
Author: Rogers M.C., Berger B.R.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology and Mineral Potential of the Upper and Middle Shebandowan Lakes Area, West-Central Shebandowan Greenstone Belt
Publication Number: OFR5938 Date: 1996
Author: Osmani I.A.
Publisher Name: Ontario Geological Survey
Location:
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