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File Created: 26-Feb-2018 by Garry J. Payie (GJP)
Last Edit:  04-Jan-2021 by Del Ferguson (DF)

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NMI
Name CAMP PORPHYRY, INEL Mining Division Liard
BCGS Map 104B066
Status Prospect NTS Map 104B10W
Latitude 056º 36' 30'' UTM 09 (NAD 83)
Longitude 130º 57' 42'' Northing 6275500
Easting 379600
Commodities Gold, Copper, Silver, Zinc Deposit Types L03 : Alkalic porphyry Cu-Au
Tectonic Belt Intermontane Terrane Stikine
Capsule Geology

The Camp Porphyry prospect is part of the INEL property, situated approximately 600 metres west of the INEL (Minfile 104B 113), approximately 9 kilometres south of Iskut River.

The Camp Porphyry zone is underlain by the Lower Jurassic Inel intrusion, comprised of feldspar porphyry intrusive rock. The intrusion is emplaced in Upper Triassic marine sedimentary and volcanic rocks of the Stuhini Group.

The Camp Porphyry is a 700 by 1400 metre area. Six drill holes completed in 2017 by Colorado Resources. Results include 0.28 gram per tonne gold and 0.08 per cent copper over 265.2 metres, including 0.59 gram per tonne gold and 0.13 per cent copper over 36 metres. (Colorado Resources, News Release, November 6, 2017).

Six drill holes, INDDH17-54, 88, 098, 099, 100 and 110 tested the Inel intrusion over a strike length of greater than 1300 metres. The results suggest that modest to low grade gold and copper mineralized zones occur over variable widths, with the strongest grades related to north-south trending structural zones and contacts between several intrusive phases or intrusive volcanic contacts. The nature of the “Camp Porphyry” has been tested over a strike distance of 1000 metres with the approximate trend of the mineralization open to the south and to the north (Assessment Report 37604).

Refer to Inel (104B 113) for work history and geological details.

Bibliography
EMPR BULL 63
EMPR EXPL 1980-467; 1983-524
EMPR FIELDWORK *1992, pp. 341-347
EMPR GEM 1972-518; 1973-501; 1974-335
EMPR GEOFILE 2015-4
EMPR GM 1997-03
EMPR INF CIRC 2015-2, p. 105
EMPR OF 1989-10; 1990-16; 1994-1; 1992-1; 1992-3; 1998-10; 2004-2; 2006-2
EMPR P 1993-1, pp. 335-339; 2004-1, pp. 1-18; 2005-1, pp. 1-30; 2006-1, pp.1-3; 2015-1, pp. 41-58
EMPR PF (See Inel - 104B 113)
EMR MP CORPFILE (Skyline Explorations Ltd.)
GSC MAP 9-1957; 311A; 1418A
GSC MEM 246
GSC P 89-1E, pp. 145-154
GCNL Oct.8, 1982; #115,#156, 1984; #86,#208, 1987; #152,#185,#245, #247, 1988; #129(Jul.6),#176(Sept.13),#179(Sept.18),#199(Oct.17),
#217(Nov.10), 1989; #139(Jul.19),#167(Aug.29),#187(Sept.27), #225(Nov.21), 1990
N MINER Jul.17, 1989; Nov.12, 1990
NAGMIN Jul.6, 1984
NW PROSP Nov./Dec. 1989
PR REL Inel Resources Ltd., May 4, Oct.28, 1987; Aug.5, Sept.23, 1988; Colorado Resources Ltd. Nov. 5, 2014; Aug. 8, 2016; Sept. 21, 2016; Dec. 19, 2016; ; May 11, Sep.12, *Nov.6, *Dec.6, 2017
PR REL Colorado Resources Ltd. *Nov. 5, 2014; Aug. 8, 2016; *Sept. 21, 2016; Dec. 19, 2016; May 11, Sep.12, *Nov.6, Dec.6, 2017; Jul. 16, 2018; Sept. 14, 2018; Sept. 16, 2020
V STOCKWATCH Sept.16,Oct.29, 1987
W MINER Feb. 1983, p. 20
Anderson, R.G. (1988): A Paleozoic and Mesozoic Stratigraphic and Plutonic Framework for the Iskut Map area (104B), Northwestern
British Columbia, pp. A1-A5, in Geology and Metallogeny of Northwestern British Columbia, Smithers Exploration Group, G.A.C. Cordilleran Section Workshop, October 16-19, 1988
Equity Preservation Corp. Stewart-Sulphurets-Iskut Compilation Dec.1988 (Showing No. B25)
Grove, E.W. (1973): Detailed Geological Studies in the Stewart Complex, Northwestern British Columbia, Ph.D. Thesis, McGill University; (1983): Report on the Inel Property in Skyline Explorations Ltd., Statement of Material Facts, March 1, 1983
Burgoyne, A.A. (2012-05-07): Technical Report on The Iskut Property with Special Reference to Johnny Flats & Burnie Trend Targets
Serensma, P.H., Johnny Mountain, A Timmins type Felsic Volcano ?
Western Miner, June 12, 1982, p. 28

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