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Currie Rose Resources Inc.
Summary
| Project: | Rossland | |
|---|---|---|
| Deposit: | Rossland | |
| Location: | Canada | |
| Commodities: | Gold-Molybdenum-Cobalt | |
| Date: | 5/28/2018 | |
| Report Code: | NI43-101 | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 28-5-2018: Currie Rose Resources Inc. announces an Exploration/Drilling Update report for its Rossland deposit at the Rossland project. Summary of previous mining and exploration on property. The Rossland mining camp is the second largest lode gold produc | |
| Resources: | x | |
| CP/QP: | [Overall Report]: Avrom Howard (Nebu Consulting LLC) | |
| ABSTRACT: | The Rossland mining camp is the second largest lode gold producing camp in British Columbia, with recovery of more than 85,900 kg (2,761,749 ounces) of gold, 109,500 kg (3,520,507 ounces) of silver and 71,502 kilograms (71 tonnes) of copper between 1894 and 1941. Vein deposits are in three main belts, referred to as the North Belt, Main Veins and South Belt. Of that, 98 percent came from the Main Veins, and 80 percent of this production came from deposits in a central core zone between two large north-trending Tertiary lamprophyre dikes. Deposits in this central zone include the Le Roi, Centre Star, Nickel Plate, Josie and War Eagle mines. A clearly defined mineralogical and chemical zonation in the camp was first recognized in the 1960s, consisting of a central zone located along the western edge of the Rossland monzonite and into the Rossland sill, dominated by massive pyrrhotite with persistent but minor chalcopyrite; an ‘intermediate’ zone, peripheral to the central zone hosting veins that contain arsenopyrite, pyrite, cobalt, bismuth minerals and molybdenite in addition to pyrrhotite and chalcopyrite; and an outer zone south of the Rossland monzonite that is marked by veins containing galena and tetrahedrite. Veins of the North Belt are entirely within the intermediate zone whereas Main Veins extend westward from the intermediate zone into the central zone. Most veins of the South Belt are within the ‘outer’ zone. Mineralization in the Rossland camp also includes molybdenite deposits on the western slopes of Red Mountain and a number of high-grade gold-quartz veins in the Sheep Creek valley and on the eastern slopes of O.K. Mountain just west of Rossland, and an area hosting a number of gold-bearing quartz-carbonate veins west of Rossland at the western edge and just north of the western edge of Currie Rose’s (henceforth referred to as the “Company”) Project. | |
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