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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  03-Jun-2021 by Garry J. Payie (GJP)

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NMI 094D8 Cr1
Name MESILINKA RIVER Mining Division Omineca
BCGS Map 094D040
Status Showing NTS Map 094D08E
Latitude 056º 23' 49'' UTM 09 (NAD 83)
Longitude 126º 05' 00'' Northing 6254077
Easting 680007
Commodities Chromium Deposit Types M05 : Alaskan-type Pt+/-Os+/-Rh+/-Ir
Tectonic Belt Intermontane Terrane Quesnel, Stikine
Capsule Geology

The Mesilinka River occurrence is located about 12 kilometres east-southeast of Dortatelle Peak (Geological Survey of Canada, Memoir 251).

The occurrence is hosted in a Late Triassic Alaskan-type ultramafic body. The ultramafic body, intruding Upper Triassic Takla Group volcanics, is approximately 2.5 kilometres in length and trends northwest (Geological Survey of Canada Open File 342). The intrusion is obliquely truncated, to the south, by a northwest trending fault. Across the fault lies the Early Jurassic Hogem batholith.

Mineralization consists of disseminated chromite within pyroxenites and peridotites as grains and rare blebs. Several seams were noted at one locale ranging in width from 1.3 to 2.5 centimetres. The chromite grains/blebs were reported to be up to 1.3 centimetres in diameter (Geological Survey of Canada Memoir 251).

The Mesilinka chromite occurrence was discovered during Geological Survey of Canada mapping program prior to 1948, under the direction of C.S. Lord. Lord published the survey's findings as Memoir 251 in 1948.

Bibliography
EMPR PF (In 094D General - *Canadian Superior Exploration Limited, Maps from Company Files, c. 1973)
GSC MEM *251
GSC MAP *962A
GSC OF 342
GSC P 76-29

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