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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  05-Jun-2023 by Karl A. Flower (KAF)

Summary Help Help

NMI 094C5 Pb3
Name TUTIZZI LEAD Mining Division Omineca
BCGS Map 094C032
Status Showing NTS Map 094C05E
Latitude 056º 18' 53'' UTM 10 (NAD 83)
Longitude 125º 42' 52'' Northing 6244418
Easting 332109
Commodities Lead, Copper Deposit Types I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Intermontane Terrane Quesnel
Capsule Geology

The Tutizzi Lead occurrence is located approximately 1 kilometre north of the western end of Tutizzi Lake, approximately 90 kilometres northwest of the community of Germansen Landing.

Regionally, the area is underlain by calc-alkaline and fine clastic sedimentary rocks of the Upper Triassic Takla Group that have been intruded by ultramafic and gabbroic to dioritic rocks of the Upper Triassic to Lower Jurassic Aiken Lake Intrusive Complex. Quartz monzonitic to monzogranitic intrusive rocks of the Lower Jurassic Hogem Plutonic Suite and monzodioritic to gabbroic intrusive rocks of the Mesilinka pluton are exposed to the southwest and south.

A lead showing is shown on Map 1030A (Geological Survey of Canada Memoir 274). No information is available on the Tutizzi lead occurrence; however, Memoir 274 (page 202) reports that "north of Tutizzi Lake, several quartz veins contain crystalline galena, commonly accompanied by chalcopyrite or specular hematite". Hostrocks are Upper Triassic Takla Group (Plughat Mountain Formation) volcanics and sediments.

Work History

During 1991 through 1994, Swannell Minerals Corp. completed programs of prospecting, geological mapping, geochemical (rock, silt and soil) sampling, a 13.1 line-kilometre ground magnetic survey, a 22.5 line-kilometre induced polarization survey and 10 diamond drillholes, totalling 897.9 metres, the area as the Abe 1-8 claims.

In 1998, Starfield Resources Inc. completed an extensive program of geological mapping, geochemical (rocks, silt and soil) sampling, a 35.8 line-kilometre ground magnetic and a 27.2 line-kilometre induced polarization survey on the Abe 1-8 and Norm 1-4 claims.

In 2004 and 2005, Commander Resources Ltd. completed programs of prospecting and geochemical (rock and soil) sampling on the Abe property. In 2007, Geoinformatics Exploration Canada Ltd. conducted a program of geological mapping, minor geochemical (rock and silt) sampling and five diamond drill holes, totalling 1600.0 metres, on the area as part of the regionally extensive Mesilinka property, which included the Abe property.

In 2012, on behalf of Commander Resources Ltd., a field program comprising reconnaissance prospecting, mapping and geochemical sampling was carried out on the Abe property. A total of 328 soil samples, 22 rock samples and 8 silt samples were collected and submitted for analysis.

During 2018 through 2021, Commander Resources Ltd. completed further programs of geological mapping and geochemical (rock and soil) sampling on the Omineca (Abe) property.

Bibliography
EMPR BULL 93
EMPR FIELDWORK 1991, pp. 127-145; 1992, pp. 109-134; 2018, pp. 31-53; 2019, pp. 25-47
EMPR GEOS MAP 2001-10
EMPR OF 1989-17; 1990-13; 1993-2; 1995-6; 1996-19
EMPR P 1992-01, pp. 127-145; 1993-01, pp. 109-134; 2019-01, pp. 31-53; 2020-01, pp. 25-47
GSC MAP 1030A
GSC MEM *274, p. 202
GSC OF 864
GBC RPT 2021-01, pp. 105-120

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