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File Created: 30-Jun-1998 by George Owsiacki (GO)
Last Edit:  24-Mar-2022 by Nicole Barlow (NB)

Summary Help Help

NMI
Name WAL, BRASSIE Mining Division Kamloops
BCGS Map 092I075
Status Showing NTS Map 092I14E
Latitude 050º 45' 02'' UTM 10 (NAD 83)
Longitude 121º 00' 52'' Northing 5623966
Easting 640066
Commodities Copper Deposit Types L04 : Porphyry Cu +/- Mo +/- Au
Tectonic Belt Intermontane Terrane Quesnel
Capsule Geology

The WAL occurrence is located 1 kilometre south of Brassy Gulch, 1.5 kilometres southwest of the community of Walhachin.

The area is primarily underlain by hydrothermally altered andesite flows and fragmental volcanic rocks of the Upper Triassic Nicola Group containing moderate to high concentrations of fine-grained, disseminated magnetite and variable amounts of pyrite. Several large limestone/marble bodies occur within the Nicola volcanics, commonly in fault contact. They strike north to northwest and are steeply dipping. A large body of hornblende diorite intrudes the Nicola Group. A smaller body of quartz porphyry intrudes both the Nicola rocks and the diorite.

In 1979, percussion drilling was completed on the Wal property to assess the mineral potential around the periphery of a gossan and to attempt to intersect a nearby mineralized intrusive breccia (Chief [MINFILE 092INW055] occurrence) that crops out on the west bank of a creek near the south part of the Wal claim. Hole W-79-1, the northernmost hole, was drilled in the bed of a creek north of the first gossan outcrop. It intersected dark-green Nicola volcanics and felsic intrusive quartz porphyry. Both units show strong pyrite mineralization with traces of chalcopyrite and malachite. Copper contents vary from 0.004 to 0.192 per cent with higher grades near the intrusive contact (Assessment Report 7736).

Work History

In 1978, Bethlehem Copper Corporation performed geological mapping, an electromagnetic survey over 5.6 kilometres and a geochemical survey. The following year, a six-hole, 597-metre percussion drilling program was carried out.

In 1999, Christopher James Gold Corp. completed a drilling and rock sampling program on the Brassie Creek property. Three drillholes, totalling 324.6 metres, were completed and 141 core samples were submitted for assay. A total of 82 rock samples were collected and submitted for assay.

In 2015, K. Ellerbeck collected 12 grab samples as part of a prospecting program on the Brassie claim group; three grab samples were assayed. In 2019 K. Ellerbeck collected 13 grab samples, four of which were submitted for assay.

Bibliography
EMPR ASS RPT 7531, *7736, 26155, 34217, 35694, 37205, 38229, 39195, 39225, 39646
EMPR BULL 56; 62
EMPR FIELDWORK 1974, pp. 27-34; 1981, pp. 270,271; 1987, pp. 417-419
EMPR MAP 7; 30
EMPR OF 1988-30; 1990-23
GSC MAP 1010A; 1386A; 42-1989
GSC MEM 262
GSC OF 165; 866; 980
GSC P 46-8; 47-10; 69-23; 73-1A, p. 212; 74-49; 82-1A, pp. 293-297; 85-1A, pp. 349-358
CJES Vol.15, No.1 (January 1978), pp. 99-116
Northcote, K.E. (1968): Geology and Geochronology of the Guichon Creek Batholith, British Columbia, Ph.D. Thesis, University of British Columbia
EMPR PFD 826934

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