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File Created: 01-Feb-2021 by Karl A. Flower (KAF)
Last Edit:  24-Mar-2022 by Nicole Barlow (NB)

Summary Help Help

NMI
Name SWAN 6, GOLDEN NEIGHBOUR 1-4 Mining Division Omineca
BCGS Map 094E035
Status Showing NTS Map 094E06E
Latitude 057º 19' 27'' UTM 09 (NAD 83)
Longitude 127º 01' 24'' Northing 6355200
Easting 619022
Commodities Gold, Silver, Copper Deposit Types
Tectonic Belt Intermontane Terrane Stikine
Capsule Geology

The Swan 6 occurrence is located at an elevation of approximately 1700 metres in the headwaters of a tributary of Saunders Creek, approximately 9.5 kilometres southwest of the west end of Toodoggone Lake.

The area lies within the Omineca-Cassiar Mountains at the southern end of the Toodoggone gold camp. It occurs within a Mesozoic volcanic arc assemblage that lies along the eastern margin of the Intermontane Belt, a northwest-trending belt of Paleozoic to Neogene sediments, volcanics and intrusions bounded to the east by the Omineca Belt and to the west and southwest by the Sustut and Bowser basins.

Permian Asitka Group crystalline limestones are the oldest rocks exposed in the region. They are commonly in thrust contact with Upper Triassic Takla Group andesite flows and pyroclastic rocks. Takla volcanics have been intruded by Lower Jurassic granodiorite to quartz monzonite of the Black Lake Suite and are in turn unconformably overlain by or faulted against Lower Jurassic calc-alkaline volcanics of the Toodoggone Formation (Hazelton Group).

The dominant structures in the area are steeply dipping faults that define a prominent regional northwest structural fabric trending 140 to 170 degrees. In turn, high-angle, northeast-striking faults (approximately 060 degrees) appear to truncate and displace northwest-striking faults. Collectively these faults form a boundary for variably rotated and tilted blocks underlain by monoclinal strata.

The occurrence area is underlain by Toodoggone Formation volcanic rocks of the upper volcanic cycle. These consist of a heterogeneous mixture of green, grey and mauve lapilli ash and lesser block tuff, with lesser interspersed ash flows and lava flows and interbedded epiclastics of the Attycelley member; partly welded, crystal-rich dacitic ash flows of the conformably overlying Saunders member and andesitic volcanic rocks of the Metsantan member.

Locally, a propylitic-altered crystal tuff hosts chalcopyrite and malachite.

In 2006, a grab sample (6187) assayed 0.330 gram per tonne gold, 22.3 grams per tonne silver and 0.519 per cent copper, whereas a chip sample (6188) over 0.4 metre yielded 0.150 gram per tonne gold, 11.2 grams per tonne silver and 0.255 per cent copper (Assessment Report 28645).

Work History

The area has been explored in conjunction with the nearby Golden Neighbour 1 and 2 (MINFILES 094E 037 and 152) occurrences and a complete exploration history can be found there.

Bibliography
EMPR BULL 86
EMPR EXPL 1975-E163-E167; 1976-E175-E177; 1977-E216-E217; 1978-E244-E246; 1979-265-267; 1980-421-436; 1982-330-345; 1983-475-488; 1984-348-357; 1985-C349-C362; 1986-C388-C414; 1987-C328-C346; 1988-C185-C194
EMPR FIELDWORK 1980, pp. 124-129; 1981, pp. 122-129, 135-141; 1982, pp. 125-127; 1983, pp. 137-138, 142-148; 1984, pp. 139-145, 291-293; 1985, pp. 167-169, 299; 1987, pp. 111, 114-115; 1989, pp. 409-415; 1991, pp. 207-216
EMPR GEM 1971-63-71; 1973-456-463
EMPR GEOLOGY 1977-1981, pp. 156-161
EMPR MAP 61 (1985)
EMPR OF 2004-4
GSC BULL 270
GSC OF 306; 483
GSC P 76-1A, pp. 87-90; 80-1A, pp. 27-32
Golden Dawn Minerals Inc. (2008-01-27): Geophysical and Diamond Drilling Report on the SWAN 1-18 Mineral
Claims, Toodoggone River Area, British Columbia

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