Ontario Geological Survey
Permanent Link to this Record:
MDI000000000695
| Record Name(s) | Eagle's Nest Project - 2010, Eagle One Deposit - 2008, Noront DDH NOT-07-05 - 2007, Double Eagle Property - 2003 |
|---|---|
| Related Record Type | |
| Related Record(s) | |
| Record Status | Developed Prospect With Reported Reserves or Resources |
| Date Created | 2009-Aug-11 |
| Date Last Modified | 2024-Apr-29 |
| Created By | |
| Revised By |
Primary Commodities: Nickel, Copper, Platinum, Palladium
Secondary Commodities: Silver, Gold
Township or Area: BMA 526 862
Latitude: 52° 44' 25.77" Longitude: -86° 17' 59.79"
UTM Zone: 16 Easting: 547262 Northing: 5843633 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 43D09NW
Point Location Description: precise
Location Method: Data Compilation
Access Description: Remote Location- Ring of Fire
2003: Noront Resources Ltd. - airborne geophysics. 2004-2006: Condor Diamond Corp. - ground geophysics. 2007-11: Noront Resources Ltd. - airborne geophysics, ground geophysics, gravity survey, and drilled 127 holes totalling 63,076 m (29 DDH in 2007, 17 DDH in 2008, 44 DDH in 2009, 34 DDH in 2010, and 3 DDH in 2011).
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| 2.29682 | 20000000351 | 20000000351 |
| 2.29749 | 20000000371 | 20000000371 |
| 2.32643 | 20000001446 | 20000001446 |
| 2.37763 | 20000003353 | 20000003353 |
| 2.37704 | 20000002819 | 20000002819 |
| 2.39940 | 20000003719 | 20000003719 |
| 2.42415 | 20000004175 | 20000004175 |
| 2.42568 | 20000000294 | 20000000294 |
| 2.45972 | 20000004813 | 20000004813 |
Province: Superior
Subprovince: Sachigo
Terrane: North Caribou
Domain: Oxford-Stull
Geological Age: Archean
| Rock Type | Rank | Composition | Texture | Relationship | Peridotite | 1 | Peridotite | Host |
|---|---|---|---|---|
| Mafic lava flow-unsubdivided | 2 | Adjacent | ||
| Granodiorite | 3 | Footwall |
Jun 02, 2017 (A Wilson) - The deposit is interpreted to be a mantle-derived ultramafic intrusion emplaced along the margin of a granodiorite pluton. The deposit is overlain by approximately 8 m of dolomitic limestone and sandstone. The deposit is a sub-vertically dipping body of massive magmatic sulphide in a pipe-like form approximately 200 m long, up to several tens of metres thick and at least 1200 m deep. It strikes northeast and occupies the northwestern margin of a vertically inclined serpentinized peridotite dyke that is present in subcrop. The present plunge of the keel of the dyke at the level of the deposit is about 70° along an azimuth of N180° from surface to a depth of 300 m.
| 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 | ||||
| 4 | Magnetite | Economic | Gangue |
Jun 02, 2017 (A Wilson) - Two styles of mineralization have been found in the deposit: massive and net-textured. Significant assays from discovery drill hole DDH NOT-07-01 are 1.84% Ni, 1.53% Cu, 1.14 g/t Pt, 3.49 g/t Pd, 0.13 g/t Au, and 4.80 g/t Ag over 36 m (from 56.0 to 92.0 m). A 4.1 m section of core from NOT-07-05 averaged 3.2% Cu, 3.62% Ni, 30.2 g/t Pt, 15.95 g/t Pd, 3.3 g/t Au, 8.1 g/t Ag, 0.84 g/t Rh, 0.15 g/t Os, 0.21g/t Ir and 0.42 g/t Ru. The massive sulphides tend to be coarse-grained with grain sizes up to 1 cm. Sometimes the pentlandite is aligned along microfractures. Medium- to very fine-grained massive sulphide veins are commonly found. These veins are often rich in silicate inclusions. The sulphides are described as massive, net-textured and disseminated. In 2009 two lenses of mixed disseminated to massive sulphides were intersected below the Eagle One Deposit in drill hole NOT-09-49. These lenses are located vertically below the deposit.
Jun 02, 2017 (Therese Pettigrew) - Other significant assays from NOT-07-05 are 4.10% Ni, 2.2% Cu, 2.09 g/t Pt, 7.13 g/t Pd, 0.42 g/t Au, and 6.30 g/t Ag over a 117.4 m length from 7.0 to 124.4 m, including 8.65% Ni, 10.90% Cu, 40.79 g/t Pt, 14.57 g/t Pd, 9.39 g/t Au, and 8.70 g/t Ag over a 3 m interval from 112.6-115.6 m (Burgess et al., 2012). Eagle’s Nest is a sub-vertically dipping body of massive magmatic sulphides (MMS) in the form of a flattened pipe approximately 200 m long and 60 m thick, and currently defined vertically to 1,650 m. The deposit remains open along strike and occupies the northwestern margin of a vertically-inclined serpentinized peridotite dyke that is present in subcrop over a north-south strike length of about 500 m with a maximum width of about 75 m. The massive sulphides within the top 250 m are confined to a volume occupying the northwestern tip of this body, and are bordered to the southeast by a thicker zone of net-textured sulphide hosted by serpentinized peridotitic cumulates. Below 250 m, the massive sulphides can be found throughout the mineralization and, in some cases, into the surrounding granodiorite. The dyke is open at the north and south ends, and plunges very steeply to the south or vertically. The exact attitude of the sulphide-filled keel at the northern tip of the dyke is impossible to state because of the irregularity of the contact. Although a considerable amount of local deformation is evident around the contacts, particularly where they are occupied by massive sulphide, the body appears to be essentially still in place and not significantly deformed. The host rock of the Eagle’s Nest ultramafic dyke is granodiorite that apparently post-dates the overlying ROF iron formation but clearly predates the intrusion of the peridotite. Because the host rocks are magnetically inert felsic rocks with little or no structural fabric and relatively low density, the intrusion is easy to recognize on magnetometer or gravimetric survey data. Inspection of the magnetometer survey results indicates that there is a second dyke parallel to and east of the Eagle’s Nest dyke, but offset en echelon to the southeast. This has been called the Eastern dyke. A third, the Southern dyke, occurs south of both of these, along strike with the Eagle’s Nest dyke (Burgess et al., 2012).
| Rank | Classification |
|---|---|
| 2 | Mafic-Ultramafic Intrusion |
| 1 | Magmatic |
| Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
|---|---|---|---|---|---|---|
| Eagle's Nest | 2012 | Proven + Probable Reserve | 11131000 | NI 43-101 09/04/2012 | Copper 0.87 %, Gold 0.18 oz/t, Nickel 1.68 %, Palladium 3.09 g/t, Platinum 0.89 g/t | |
| Eagle's Nest Main Zone | 2012 | Measured + Indicated Resource | 11000000 | NI 43-101 (09/04/2012) | 1.78% Ni, 0.98% Cu, 0.99 g/t Pt, 3.41 g/t Pd, 0.20 g/t Au | Copper 0.98 %, Gold 0.2 oz/t, Nickel 1.78 %, Palladium 3.41 g/t, Platinum 0.99 g/t |
| Eagle's Nest Main Zone | 2012 | Inferred Mineral Resource | 8966000 | NI 43-101 (09/04/2012) | 1.10% Ni, 1.14% Cu, 1.16 g/t Pt, 3.49 g/t Pd, 0.30 g/t Au | Copper 1.14 %, Gold 0.3 oz/t, Nickel 1.10 %, Palladium 3.49 g/t, Platinum 1.16 g/t |
| Eagle's Nest East Zone | 2012 | Inferred Mineral Resource | 1615000 | NI 43-101 (09/04/2012) | 0.34% Ni, 0.09% Cu, 0.12 g/t Pt, 0.45 g/t Pd, 0.04 g/t Au | Copper 0.09 %, Gold 0.04 oz/t, Nickel 0.34 %, Palladium 0.45 g/t, Platinum 0.12 g/t |
| Eagle's Nest | 2012 | Inferred Mineral Resource | 8966000 | NI 43-101 (09/04/2012) | 1.10% Ni; 1.14% Cu, 1.16 g/tonne Pt; 3.49 g/tonne Pd, 0.3 oz/t | Copper 1.14 %, Gold 0.3 oz/t, Nickel 1.10 %, Palladium 3.49 g/t, Platinum 1.16 g/t |
| Eagle's Nest | 2012 | Probable Mineral Reserve | 5867000 | NI 43-101 (09/04/2012) | 1.38% Ni; 0.72% Cu, 1.01 g/tonne Pt; 3.45 g/tonne Pd, 0.18 oz/t Au | Copper 0.72 %, Gold 0.18 oz/t, Nickel 1.38 %, Palladium 3.45 g/t, Platinum 1.01 g/t |
| Eagle's Nest | 2012 | Proven Mineral Reserve | 5264000 | NI 43-101 09/04/2012 | 2.02% Ni; 1.04% Cu; 1.01 g/tonne Pt; 3.45 g/tonne Pd; 0.18 oz/t Au | Copper 1.04 %, Gold 0.18 oz/t, Nickel 2.02 %, Palladium 3.45 g/t, Platinum 1.01 g/t |
| Eagle’s Nest | 2010 | Indicated Mineral Resource | 6900000 | Baker et al. Technical Report Eagle's Nest Project | Copper .95 %, Nickel 2.04 %, Palladium 3.4 g/t, Platinum 1.3 g/t | |
| Eagle’s Nest | 2010 | Inferred Mineral Resource | 4300000 | Baker et al. Technical Report Eagle's Nest Project | Copper .87 %, Nickel 1.42 %, Palladium .8 g/t, Platinum 3.4 g/t | |
| Eagle One | 2008 | Indicated Mineral Resource | 1834000 | P & E Mining Consultants 2008, Technical Report Eagle One Deposit | 79.2 million lbs Ni, 47.6 million lbs Cu, 9100 oz Au, 6,200 oz Pt, 230,500 oz Pd and 224,400 oz Ag | Copper 1.18 %, Gold .15 g/t, Nickel 1.96 %, Palladium 3.91 g/t, Platinum 1.12 g/t, Silver 3.81 g/t |
| Eagle One | 2008 | Inferred Mineral Resource | 1087000 | P & E Mining Consultants 2008, Technical Report Eagle One Deposit | 57.2 million lbs Ni, 30.5 million lbs Cu, 4600 oz Au, 47,900 oz Pt, 157,300 oz Pd and 147,000 oz Ag | Copper 1.27 %, Gold .13 g/t, Nickel 2.39 %, Palladium 4.5 g/t, Platinum 1.37 g/t, Silver 4.21 g/t |
Publication - Technical report and preliminary economic assessment on the Eagle One Deposit, Double Eagle Property, McFaulds Lake Area, James Bay Lowlands, Ontario, 108p.
Publication Number: NI 43-101 Date: 2008
Author: T. Armstrong, E. Puritch, A. Yassa, J.L. Pearson, A. Hayden and A. Partsch
Publisher Name:
Location: Timmins RGO files
Map - Precambrian Geology of the Hudson Bay and James Bay Lowlands Region Interpreted from Aeromagnetic Data-East Sheet
Publication Number: P3598-REV Scale: 1:500,000 Date: 2008
Author: Stott G.M.
Publisher Name: Ontario Geological Survey
Location:
Publication - Technical report and resource estimate on the Eagle One Deposit, Double Eagle Property, McFaulds Lake Area, James Bay Lowlands, Ontario, 108p.
Publication Number: NI 43-101 Date: 2008
Author: T. Armstrong, E. Puritch, A. Yassa, J.L. Pearson, A. Hayden and A. Partsch
Publisher Name:
Location: Timmins RGO library
Publication - Technical report,preliminary economic assessment McFaulds Lake Property, Eagle's Nest Project, James Bay Lowlands, Ontario, 136p.
Publication Number: NI 43-101 Date: 2010
Author: S. Baker, H. Burgess, R. Gowans, G. Greenough, C. Jacobs, C. Murahwi and P.
Publisher Name:
Location: Timmins RGO
Map - Precambrian Geology of the Hudson Bay and James Bay Lowlands Region Interpreted from Aeromagnetic Data-South Sheet
Publication Number: P3599-REV Scale: 1:500,000 Date: 2009
Author: Stott G.M.
Publisher Name: Ontario Geological Survey
Location:
Mono - Mineral Deposits of Northern Ontario, North of Latitude 49° 30'
Publication Number: OFR6242 Date: 2009
Author: Stott G.M., Josey S.D.
Publisher Name: Ontario Geological Survey
Location:
Publication - Feasibility study on the Eagle's Nest Deposit, McFaulds Lake Area, James Bay Lowlands, Ontario.
Publication Number: NI 43-101 FS Date: 2012
Author: R. Gowans (2012)
Publisher Name:
Location: SEDAR
Publication - Feasibility study on the Eagle's Nest Deposit, McFaulds Lake Area, James Bay Lowlands, Ontario, 210 p.
Publication Number: NI 43-101 Date: 2012
Author: H. Burgess, R. Gowans , C. Jacobs, C. Murahwi, B. Damjanovic
Publisher Name:
Location:
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