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File Created: 27-Nov-1995 by Garry J. Payie (GJP)
Last Edit:  28-Mar-2022 by Nicole Barlow (NB)

Summary Help Help

NMI 104I7 Cu1
Name NORTHWEST, TURN, COBALT, PYRRHOTITE, CUB, TURNAGAIN, BENCH Mining Division Liard
BCGS Map 104I046
Status Prospect NTS Map 104I07W
Latitude 058º 28' 29'' UTM 09 (NAD 83)
Longitude 128º 51' 55'' Northing 6481572
Easting 507858
Commodities Copper, Nickel, Molybdenum Deposit Types M05 : Alaskan-type Pt+/-Os+/-Rh+/-Ir
Tectonic Belt Intermontane Terrane Cache Creek, Cassiar, Quesnel
Capsule Geology

The Northwest (Turn) occurrence is located about 68 kilometres east of Dease Lake.

The occurrence is hosted in an Alaskan-type ultramafic intrusive complex. This zoned complex consists of a dunite core and surrounding peripheral peridotites, pyroxene-rich peridotite, and olivine pyroxenite with maximum dimensions of 3 by 8.2 kilometres. It was intruded in the Lower Jurassic (and earlier(?)) into Upper Paleozoic(?) and/or Triassic(?) metavolcanic and metasedimentary rocks of the Quesnel Terrane. It is in faulted contact on the east and north with slate and phyllite of the Ordovician to Mississippian Road River Group (Ancestral North America).

The Northwest showing occurs in rusty weathering peridotites with minor concentrations of interstitial pyrrhotite and chalcopyrite to about 10 per cent, and as small, massive pods. The rocks appear to form an alternating sequence of dunites, peridotites and olivine pyroxenites.

Several diamond-drill and pack-sack holes were put down in and around the Northwest area by Falconbridge Nickel Mines, probably in 1970 (Assessment Report 3735, Map 4). Results from these holes are not published. However, Supreme Resources resampled the core of a number of these drillholes and published some of the assays. A 1.83-metre section of diamond-drill hole 28 assayed (at 68.88 metres depth) 1.12 per cent nickel, 1.72 per cent molybdenite and 0.2 per cent copper (Assessment Report 16458 (drill logs)).

In 2004, three holes on the Northwest zone included broader intervals (4.0 to 26.5 metres) grading between 0.27 and 0.35 per cent nickel (Technical Report on the 2004 Exploration Program - June 15, 2005, N.C. Carter, for Hard Creek Nickel Corporation, http://www.hardcreeknickel.com).

The Northwest Zone is contiguous with, and lies northwest of, the Horsetrail Zone. This zone has mineralization styles and grades similar to the Horsetrail Zone but is intruded by several mafic and felsic dikes which dilute the overall grade. Drill core samples from the Northwest Zone have a median grade of 0.20 per cent total nickel with grades ranging from 0.01 to 2.86 per cent; sulphide nickel-based grades range from 0.01 to 0.76 per cent and have a median of 0.14 per cent (Preliminary Economic Assessment, December 2, 2011). Total cobalt grades range from 0.001 to 0.166 per cent (Preliminary Economic Assessment, December 2, 2011). The Horsetrail and the Northwest Zones form a zone approximately 2,000 metres long in the east-west direction, and 550 metres wide from north to south and have been tested by 228 drillholes.

See Turnagain Nickel (Horsetrail) (104I 119) for further details of the Turnagain property, including geology, work history and bibliography.

Bibliography
EMPR AR 1966-22; 1967-28
EMPR EXPL 1979-484; 1987-384,385; 1999-19-31; 2003-8,9; 2004-26,27
EMPR GEM 1969-49; 1970-40; 1971-46; 1972-545; 1973-512
EMPR MER 2003-20; 2004-13
EMPR OF 1989-18; 1996-11
EMPR PF (in 104I 014 file - Kilburn, L.C. (1967): Report on Turnagain Copper-Nickel Prospect to December 1967)
GSC BULL 504
GSC MAP 9-1957; 29-1962; 1418A; 1712A
GSC OF 610; 2262; 2779
GSC P 78-1A, pp. 25-27
PR REL Canadian Metals Exploration: Sept.17, Oct.15,24, Nov.14, Dec.12, 2002; Feb.20, Mar.19, Apr.7,28, May 30, July 29, Sept.25, Oct.21,30, Nov.12,28 Dec.4, 2003; Mar.8, Apr.26 May 11, June 25, 2004; Hard Creek Nickel Corp: May 8, Aug.9, Sept.12,15,23, Nov.14,17, Dec.8,13, 2004; July 7, Sept.9,26, Oct.31, 2005; Jun.15,21; Jul.17, Dec.13,21, 2006; Jan.10, 2007; Nov.26, 2008; May 5, 2009; Apr.9,12, Nov.1, 2010; Jan.5, Mar.16, Apr.7, Oct.20, 2011; Giga Metals Corp., Jan.30, Feb.25, 2019
CJES *Vol.15, No.12, 1978, pp. 1893-1903; *Vol.17, No.6, 1980, pp. 744-757
*Clark, T. (1975): Geology of an ultramafic complex on the Turnagain River, northwestern British Columbia. Ph.D. thesis, Queen's University, Kingston, Ontario
Simpson, R.G. (2007-03-29): Mineral Resource Update – Turnagain Nickel Project
Kulla, G. (2007-09-25): NI 43-101 Technical Report on Preliminary Assessment - Turnagain Nickel Project
Wells, P. (2010-04-07): Technical Report on the Turnagain Project
*Riles, A., Molavi, M. (2011-12-02): Preliminary Economic Assessment – Turnagain Project
Nixon, G.T., Milidragovic, D. and Scoates, J.S., Convergent margin Ni-Cu-PGE-Cr ore systems: temporal and magmatic evolution, Targeted Geoscience Initiative 5, Grant Program Interim Reports 2018-2019
Falconbridge File
Gigametals Corporation (2020-11-18): N.I. 43-101 Technical Report & Preliminary Economic Assessment for the Turnagain Project, British Columbia, Canada
Gigametals Corporation (2021-02-03): N.I. 43-101 Technical Report & Preliminary Economic Assessment for the Turnagain Project - Amended

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