British Columbia Ministry of Energy, Mines and Natural Gas and Responsible for Housing
News | The Premier Online | Ministries & Organizations | Job Opportunities | Main Index

MINFILE Home page  ARIS Home page  MINFILE Search page  Property File Search
Help Help
File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  24-May-1991 by Garry J. Payie (GJP)

Summary Help Help

NMI 082F3 Zn7
Name JACKPOT EAST, JACKPOT, EAST, JACK POT, TWO SPOT Mining Division Nelson
BCGS Map 082F025
Status Developed Prospect NTS Map 082F03E
Latitude 049º 14' 38'' UTM 11 (NAD 83)
Longitude 117º 08' 48'' Northing 5454579
Easting 489325
Commodities Zinc, Lead, Tungsten Deposit Types E12 : Mississippi Valley-type Pb-Zn
E13 : Irish-type carbonate-hosted Zn-Pb
Tectonic Belt Omineca Terrane Kootenay, Plutonic Rocks
Capsule Geology

The Jackpot East prospect is located on the ridge between Hidden and Porcupine creeks, 10 kilometres northeast of Salmo. See also Jackpot Main (082FSW012), Jackpot West (082FSW255) and Jackpot Lerwick (082FSW256).

The Jackpot orebodies are currently thought to be Kootenay Arc-type carbonate hosted sedimentary exhalative (sedex) deposits. The orebodies are located within dolomitized limestone of the Lower Cambrian Laib Formation, Reeves Member (correlative with limestone of the Badshot Formation). In the occurrence area, the host Reeves Member is complexly folded and faulted and is in close proximity to the north margin of the Hidden Creek stock of the Middle to Late Jurassic Nelson Intrusions.

The carbonates form the core of the Jackpot syncline which trends slightly northeast and dips about 60 degrees east above 1370 metres elevation. Below this elevation the dip changes through vertical to west dipping. The core carbonates are underlain by brown biotite hornfels and white to brown, micaceous limestone of the Truman Member of the Laib Formation and by fine grey micaceous quartzites of the Lower Cambrian Reno Formation. The hornfels is locally altered to a banded diopside rock and the limestones are locally altered to skarn and reportedly carry scheelite. The east limb of the syncline is in fault contact with the Ordovician Active Formation argillites.

The Jackpot East mineralization consisting of pyrite, pyrrhotite, sphalerite, and minor galena is confined to bands of dolomite up to about 3 metres thick which alternate with barren dolomites. Sulphides are disseminated and grade ranges from 3 to 15 per cent zinc and minor lead (Bulletin 41). The mineralized zone including barren horizons is in the order of 30 metres thick although individual mineralized horizons have not proven to be laterally extensive. The occurrence has had extensive exploration work but no significant production has been documented. For reserves and work history refer to Jackpot Main (082FSW012).

Tombstone Explorations Co. Ltd. acquired the Jackpot property from New Jersey Zinc Explorations Company (Canada) Ltd. in 1997.

Bibliography
EMPR AR 1948-132; *1949-165; 1951-136,236; 1952-145; 1953-115; 1954-125; 1956-78; 1965-180; 1966-212; 1968-241
EMPR ASS RPT *6250, 9785, 10602, 10883, 10885, 11163, *11450
EMPR BULL *41, pp. 121-126; 109
EMPR EXPL 1975-E31; 1976-E34; 1977-E43; 1982-45,46; 1983-52
EMPR FIELDWORK 1987, pp. 19-30; 1988, pp. 33-43; 1989, pp. 11-27; 1990, pp. 9-31
EMPR GEM 1973-58; 1974-68; 1975-E31; 1976-E34
EMPR OF 1988-1; 1989-11; 1990-8; 1990-9; 1991-2; 1991-17; 2000-22
EMPR PF (Surface Geological Plan of the Jackot-East Showing, New Jersey Zinc Explorations Ltd., 1951; East-West Sections of 4500N and 4800N, New Jersey Zinc Exploration Co. Ltd., 1955; (also see Jackpot Main - 082FSW012))
EMR MP CORPFILE (Tri Basin Resources Ltd.; New Jersey Zinc Exploration Company (Canada) Ltd.)
GSC BULL 29-9
GSC MEM 94; 172; 308
GSC OF 1195
GSC P 50-19; 51-4
GCNL #32, 1982; Sept.27, 1983
N MINER March 4, 1982
Tri Basin Resources Ltd., Filing Statement, 1984

COPYRIGHT | DISCLAIMER | PRIVACY | ACCESSIBILITY