Ontario Geological Survey
Permanent Link to this Record:
MDI42A06SE00065
| Record Name(s) | Hart Deposit - 1979, Hart Prospect - 1964, Paramaque DDH 64-5 - 1964 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Developed Prospect With Reported Reserves or Resources |
| Date Created | 1983-Oct-07 |
| Date Last Modified | 2022-Sep-19 |
| Created By | |
| Revised By |
Primary Commodities: Copper, Nickel
Secondary Commodities: Palladium, Platinum, Gold
Township or Area: Eldorado
Latitude: 48° 18' 13.37" Longitude: -81° 4' 51.66"
UTM Zone: 17 Easting: 493992.002 Northing: 5350060.998 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42A06SE
Point Location Description: precise
Location Method: Data Compilation
Access Description: The property is accessed from the city of Timmins by a series of gravel roads. Approximately twenty-six kilometres southeast of Timmins, a road branches east to the Hart property. Approximately three kilometres east along this road the deposit location is reached.
pre 1964: T. N. Hart - trenching, sampling. 1964-68: Norlex Mines Limited - ground geophysics, 13 ddh (1854.4 m). 1968: Paramaque Mines Ltd. - 6 ddh (1959 m). 1969: McWatters Gold Mines Ltd. - optioned property, 8 ddh (2440 m). 1989: Timmins Nickel inc. - airborne geophysics, ground geophysics. 2001: Hucamp Mines Limited - property optioned. 2002: Starfire Minerals Inc. - 6 ddh (471.08 m). 2004: Canadian Arrow Mines - property acquisition, ground geophysics, DD-5-306 m. 2003- 2011: Liberty Mines Inc. - airborne geophysics, DD-104-301 m, trenching. 2012: Liberty Mines Inc. - DD-8-4579m. 2013: Liberty Mines changed its name to Northern Sun Mining Corp.
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| T-4953 / 2.26599 | 42A07SW2012 | 42A07SW2012 |
| T-4827 / 2.24937 | 43B12NW2007 | 43B12NW2007 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Geological Age: Neoarchean
| Rock Type | Rank | Composition | Texture | Relationship | Peridotite | 1 | Serpentinized Peridotite | Contains |
|---|---|---|---|---|
| Ironstone-unsubdivided | 2 | Footwall | ||
| Felsic Tuff-Breccia | 3 | Tuff, Breccia | Footwall | |
| Ultramafic lava flow-unsubdivided | 4 | Komatiite | Ortho To Mesocumulate | Host |
Jul 14, 2010 (A Wilson) - The serpentinized peridotite hosting the mineralization is massive and locally altered to chlorite, carbonate and talc. Primary cumulate textures are not obvious in hand specimen. Spinifex textures are absent in the basal ultramafic unit hosting the mineralization, but pyroxenite and olivine spinifex are reported in the pyroxenitic and ultramafic flows. The structural and stratigraphic footwall consists of intermediate to felsic volcanic breccia and tuff and sulphide-bearing iron formation which locally overlies the breccia. At a vertical depth of 150 m the iron formation pinches out and the peridotite and volcanic breccia are in contact. The komatiitic rocks, which host the mineralization are serpentinized and locally altered to talc, chlorite and carbonate. Spinifex textures are common, occurring at distinct stratigraphic horizons, serving as a tentative marker horizon.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Pyrrhotite | Economic | Ore | ||||
| 2 | Pentlandite | Economic | Ore | ||||
| 3 | Chalcopyrite | Economic | Ore | ||||
| 1 | Pyrite | Economic | Gangue | ||||
| 2 | Magnetite | Economic | Gangue | ||||
| Serpentine | Alteration | Serpentinization | 1 | Unknown | Replacement | ||
| Chlorite | Alteration | Carbonatization | 2 | Unknown | Disseminated |
Jul 14, 2010 (A Wilson) - Assays from the diamond drilling completed by Paramaque returned values ranging from 0.30% Ni to 2.77% Ni. An assay of 2.77% Ni and 0.13% Cu over 3.6m was returned from a Paramaque drill hole 64-4. Reported assays from the Noralex drilling returned assays as high as 2.10% Ni over 4.57 m. The best assays for diamond drilling completed by Starfire returned: 0.044% Cu, 0.59% Ni, 0.1 g/t Pt, 0.11 g/t Pd over 1.28 m in drill hole SH02-02l 0.06% Cu, 0.67% Ni, 0.18 g/t Pt and 0.28 g/t Pd over0.71 m from SH-02-05. The contained sulphide minerals in decreasing abundance are: pyrrhotite, pentlandite, minor pyrite and chalcopyrite, occurring predominantly as massive to semi-massive sulphides at the base of the komatiitic flow. The total sulphide abundance decreases with increasing distance from the basal contact. The main zone that comprises the majority of the mineral resource consists of komatiite-hosted massive to semi-massive sulphides lying conformably on dacitic pyroclastic flows. The sulphide assemblage consists of pyrrhotite, pentlandite, and minor pyrite and chalcopyrite. Typical sulphide concentrations range in the sixty to eighty percent pyrrhotite and ten to thirty percent pentlandite. The pentlandite occurs intergrown with pyrrhotite as irregular grains that are generally relatively coarse grained. The massive zone is overlain by disseminated sulphides of varying sulphide modal abundance, ranging from under one percent to twenty-five%. The sulphide minerals are similar to those of the massive zone, with the exception of minor amounts of millerite also identified in thin section. Silicate minerals have been completely serpentized and/or carbonatized.
| Rank | Classification |
|---|---|
| 2 | Mafic-Ultramafic Intrusion |
| 1 | Magmatic |
| Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
|---|---|---|---|---|---|---|---|---|---|
| Tabular | 213 | 9 | 300 | 50 |
Date: Jul 08, 2003
Geologist: A Wilson
Notes: The mineralized zone occurs along the footwall peridotite contact overlying the pyroclastic rocks and sulphide iron formation. The zone plunges 50 degrees SE, parallel to the plunge of broad open cross folds on the northern limb of the syncline. Irregularly shaped and discontinuous pods of mainly massive iron sulphides occur along the contact between the volcanic breccia, iron formation and peridotite contact. These massive pods are overlain by blebby or disseminated sulphides representing original net-textured sulphides.
| Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
|---|---|---|---|---|---|---|
| Hart Deposit | 2012 | Indicated Mineral Resource | 1546000 | NI 43-101 rpt, p. 1-6 | 47,779,000 lbs contained Ni | Copper 0.10 Percent, Nickel 1.40 Percent |
| Hart Deposit | 2012 | Inferred Mineral Resource | 322000 | NI 43-101 rpt, p. 1-6 | 8,990,000 lbs contained Ni | Copper 0.08 Percent, Nickel 1.27 Percent |
| IF Zone | 2010 | Indicated Mineral Resource | 120000 | NI 43-101 rpt, p. 62 | @ 0.70% Ni, 0.06% Cu, 1,850,000 lbs contained Ni | Copper .06 Percent, Nickel .7 Percent |
| Upper Massive Zone | 2010 | Inferred Mineral Resource | 59000 | NI 43-101 rpt, p. 62 | @ 1.12% Ni, 0.08% Cu, 1,466,000 lbs contained Ni | Copper .08 Percent, Nickel 1.12 Percent |
| Upper Disseminated Zone | 2010 | Indicated Mineral Resource | 14000 | NI 43-101 rpt, p. 62 | @ 0.50% Ni, 0.03% Cu, 152,000 lbs contained Ni | Copper .03 Percent, Nickel .5 Percent |
| IF Zone | 2010 | Inferred Mineral Resource | 12000 | NI 43-101 rpt, p. 62 | @ 0.86% Ni, 0.07% Cu, 225,000 lbs contained Ni | Copper .07 Percent, Nickel .86 Percent |
| Upper Massive Zone | 2010 | Indicated Mineral Resource | 353000 | NI 43-101 rpt, p. 62 | @ 1.36% Ni, 0.09% Cu, 10,588,000 lbs contained Ni | Copper .09 Percent, Nickel 1.36 Percent |
| Lower Disseminated Zone | 2010 | Inferred Mineral Resource | 22000 | NI 43-101 rpt, p. 62 | @ 0.52% Ni, 0.02% Cu, 255,000 lbs contained Ni | Copper .02 Percent, Nickel .52 Percent |
| Lower Disseminated Zone | 2010 | Indicated Mineral Resource | 60000 | NI 43-101 rpt, p. 62 | @ 0.63% Ni, 0.04% Cu, 838,000 lbs contained Ni | Copper .04 Percent, Nickel .63 Percent |
| Lower Massive Zone | 2010 | Inferred Mineral Resource | 228000 | NI 43-101 rpt, p. 62 | @ 1.40% Ni, 0.09% Cu, 7,044,000 lbs contained Ni | Copper .09 Percent, Nickel 1.4 Percent |
| Lower Massive Zone | 2010 | Indicated Mineral Resource | 999000 | NI 43-101 rpt, p. 62 | @ 1.56% Ni, 0.11% Cu, 34,352,000 lbs contained Ni | Copper .11 Percent, Nickel 1.56 Percent |
| Hart Nickel Project | 2008 | Indicated Mineral Resource | 1390000 | Liberty Mines Inc., press release, June 23, 2008 | 45,972,000 lbs contained Ni | Copper .1 Percent, Nickel 1.5 Percent |
| Hart Nickel Project | 2008 | Inferred Mineral Resource | 286000 | Liberty Mines Inc., press release, June 23, 2008 | 8,572,000 lbs contained Ni | Copper .09 Percent, Nickel 1.36 Percent |
| HART PROSPECT | 1999 | Unclassified | 770000 | RESIDENT GEOLOGIST FILES | Nickel .9 Percent |
File - Resident Geologist files T-1430
Publication Number: Date:
Author:
Publisher Name:
Location: Timmins RGP office
Map - Adams and Eldorado townships, Timiskaming District
Publication Number: M2274 Scale: 1:31,680 Date: 1974
Author: Pyke D.R.
Publisher Name: Ontario Division of Mines
Location:
Map - Timmins, Precambrian geology
Publication Number: M2455 Scale: 1:50,000 Date: 1982
Author: Pyke D.R.
Publisher Name: Ontario Geological Survey
Location:
Publication - Northern Miner, 1968, Sept. 19
Publication Number: NMINER Date: 1968
Author:
Publisher Name: Northern Miner
Location: Timmins RGO
Map - Eldorado Township, District of Timiskaming
Publication Number: P0572 Scale: 1:15,840 Date: 1997
Author: Pyke D.R.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Timmins data series, Eldorado Township, District of Cochrane
Publication Number: P2114 Scale: 1:15,840 Date: 1980
Author: Hunt D.S., MacRae B.A., Maharaj D.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological Compilation of the Timmins Area, Abitibi Greenstone Belt
Publication Number: P3379 Scale: 1:100,000 Date: 1998
Author: Ayer J.A., Trowell N.F.
Publisher Name:
Location:
Mono - Copper, nickel, lead and zinc deposits of Ontario
Publication Number: MDC012 Page: 355-356 Date: 1969
Author: Shklanka R.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Distribution and characteristics of the sulphide ores of the Timmins area
Publication Number: MP041 Page: 20 Date: 1970
Author: Pyke D.R., Middleton R.S.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of Adams and Eldorado townships, District of Cochrane
Publication Number: R121 Page: 35-37 Date: 1975
Author: Pyke D.R.
Publisher Name: Ontario Division of Mines
Location:
Mono - Nickel sulphide deposits associated with ultramafic rocks of the Abitibi belt and economic potential of mafic-ultramafic intrusions
Publication Number: S020 Page: 32-35 Date: 1979
Author: Coad P.R.
Publisher Name: Ontario Geological Survey
Location:
Book - Hucamp Mines Limited
Publication Number: clippings Date: 2001
Author:
Publisher Name:
Location: Timmins RGO
Thesis - A petrological study of the ultramafic and related rocks of the Shaw Dome, southeast of Timmins, Ontario
Publication Number: MSc Thesis Page: 184-190 Date: 1975
Author: Muir, T.L.
Publisher Name: Queen's University
Location: Timmins RGP Office
Publication - Liberty receives resource estimate for the Hart Nickel Project
Publication Number: clipping Date: 2008
Author: Liberty Mines Inc.
Publisher Name:
Location: Timmins clipping files
Publication - Preliminary Economic Assessment for the Hart Project, 152p.
Publication Number: NI 43-101 rpt Date: 2010
Author: G. Cole, A. Mackenzie, P. Bridson, W. Randall
Publisher Name:
Location: Timmins RGO
Publication - Hart Project - Preliminary Economic Assessment, 548p.
Publication Number: Date: 2012
Author: M. Hatton, G. Cole
Publisher Name:
Location: Timmins RGO
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