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File Created: 15-Dec-1992 by Garry J. Payie (GJP)
Last Edit:  26-May-2021 by George Owsiacki (GO)

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NMI
Name JUMP Mining Division Omineca
BCGS Map 094C041
Status Showing NTS Map 094C05W
Latitude 056º 28' 06'' UTM 10 (NAD 83)
Longitude 125º 55' 45'' Northing 6262052
Easting 319560
Commodities Copper Deposit Types L04 : Porphyry Cu +/- Mo +/- Au
Tectonic Belt Intermontane Terrane Quesnel
Capsule Geology

The Jump occurrence is located about 9.6 kilometres northwest of Aiken Lake and approximately 108 kilometres northwest of the community of Germansen Landing.

The Jump showing consists of minor occurrences of malachite and possibly chalcopyrite hosted in a flow of augite/feldspar porphyry agglomerate of the Upper Triassic Plughat Mountain Formation (Takla Group). The mineralization appears to be related to a mafic-rich marginal phase of a hornblende porphyry dike which cuts the Takla rock. There is some local shearing but its association with the mineralization is unclear.

In 1992, a grab sample of the mineralization taken for analysis yielded 0.48 per cent copper, 0.015 gram per tonne gold, 0.021 per cent zinc and 0.013 per cent lead (Open File 1993-2, Map Number 32).

Bibliography
EMPR ASS RPT 35191
EMPR FIELDWORK 1991, pp. 127-145; *1992, pp. 109-134; 2018, pp. 31-53; 2019, pp. 25-47
EMPR P 1992-01, pp. 127-145; 1993-01, pp. 109-134; 2019-01, pp. 31-53; 2020-01, pp. 25-47
EMPR OF 1992-11; *1993-2
EMPR PFD 673269
GBC 2021-01, pp. 105-120
GSC MEM 274
GSC MAP 1030A

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