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: 15-Jun-2015 by Karl A. Flower (KAF)
Last Edit:  05-Sep-2023 by Garry J. Payie (GJP)

Summary Help Help

NMI
Name SAINT JOE 9, BERT, JACK, SJ04-1, ST. JOE 9 Mining Division Fort Steele
BCGS Map 082G041
Status Showing NTS Map 082G05W
Latitude 049º 29' 41'' UTM 11 (NAD 83)
Longitude 115º 53' 25'' Northing 5483046
Easting 580360
Commodities Silver, Cobalt, Copper Deposit Types I06 : Cu+/-Ag quartz veins
Tectonic Belt Omineca Terrane Ancestral North America
Capsule Geology

The Saint Joe 9 occurrence is located on a ridge separating Jim Smith and Kiakho creeks, approximately 1.2 kilometres east of the north end of Kiakho Lakes.

The area is underlain by metasediments of the Middle Proterozoic Purcell Supergroup, Creston Formation. The rocks are intruded by rocks of the mid-Cretaceous Bayonne plutonic suite. In addition to the numerous typically granodiorite intrusives representing the Bayonne plutonic suite, much more alkaline syenite and quartz syenite intrusives (stocks and dikes) occur in this area.

Locally, a zone of intense silicification, chloritization and brecciated is identified by diamond drilling. The zone follows the Cranbrook fault, which has thrown Creston Formation rocks into contact with Aldridge Formation sediments, both formations of the Helikian Purcell Supergroup. The controlling fault has a general east strike and steep northerly dip. The brecciated quartzites are intensely silicified and chloritized with quartz veins hosting massive pyrite and chalcopyrite.

In 2004, diamond drill hole SJ04-1 intercepted 1.0 metre averaging 4.5 grams per tonne silver, 0.032 per cent cobalt and 1.06 per cent copper (Sample 87288; Assessment Report 27764).

In 1966, Rimrock Minerals completed a 55.7 line-kilometre ground magnetic survey in the area (Assessment Report 895). In 1967, Vanco Explorations completed a 26.0 line-kilometre ground magnetic survey on the area as the Jack claims (Assessment Report 1007). In 1967, Placid Oil completed a program of geological mapping, a 160.0 line-kilometre induced polarization survey and a 33.6 line-kilometre ground magnetic survey in the area (Assessment Reports 1174, 1178). In 1993, Consolidated Ramrod Gold completed four diamond drill holes, totalling 636.0 metres, in the area (Assessment Report 23135). In 2004, Klondike Gold completed two diamond drill holes, totalling 341.7 metres, in the area (Assessment Report 27764).

In 1966, Rimrock Minerals completed a 55.7 line-kilometre ground magnetic survey on the area. In 1967, Vanco Explorations completed a 26.0 line-kilometre ground magnetic survey on the area as the Jack claims. Also in 1967, Placid Oil completed a program of geological mapping, a 160.0 line-kilometre induced polarization survey and a 33.6 line-kilometre ground magnetic survey. In 2004, Klondike Gold completed two diamond drill holes, totalling 341.7 metres, on the area.

In 2013/2014, PJX Resources Inc began a large program of gravity and magnetic geophysical surveying to detect dense subsurface features (Assessment Reports 34082, 34937, 35416). The gravity survey extended 10 kilometres beyond the West Basin property claim boundaries encompassing several MINFILE occurrences including the Saint Joe 9 (Figure 8, Assessment Report 34082).

Bibliography
EMPR ASS RPT 895, 1007, 1174, 1178, 11570, 20472, 23135, *27764, 34082, 34937, 35416
EMPR FIELDWORK 1983, pp. 24-35
EMPR GEOS MAP 1998-3
EMPR OF *1988-14
EMPR PFD 676659
GSC MAP 11-1960

COPYRIGHT | DISCLAIMER | PRIVACY | ACCESSIBILITY