The Geology and Mineralization of the Coquihalla Gold Belt and Hozameen Fault System, Southwestern British Columbia

The Geology and Mineralization of the Coquihalla Gold Belt and Hozameen Fault System, Southwestern British Columbia

Author: Gerald E. Ray

Publisher: Province of British Columbia, Ministry of Energy, Mines and Petroleum Resources

Published: 1990

Total Pages: 116

ISBN-13:

DOWNLOAD EBOOK

Description of the geology, gold deposits and mineral occurrences adjacent to the Hozameen fault system and Coquihalla serpentine belt in southwestern B.C. The report gives a general geology of the area, the structural geology, and the economic geology by mine or gold occurrence. A short description of other mineral occurrences is also given.


From the Puget Lowland to East of the Cascade Range

From the Puget Lowland to East of the Cascade Range

Author: Ralph A. Haugerud

Publisher: Geological Society of America

Published: 2017-10-13

Total Pages: 264

ISBN-13: 0813700493

DOWNLOAD EBOOK

"This volume contains guides that geographically focus on the Seattle, Washington, area within the Puget lowland, and also includes descriptions of trips in the Cascade Range and the region east of the Cascades"--


Ore Deposits, Tectonics, and Metallogeny in the Canadian Cordillera

Ore Deposits, Tectonics, and Metallogeny in the Canadian Cordillera

Author: W. J. McMillan

Publisher: Province of British Columbia, Mineral Resources Division

Published: 1991

Total Pages: 294

ISBN-13:

DOWNLOAD EBOOK

This report provides a tectonic and mineral deposit overview, then discusses deposits in North American rocks, followed by deposits formed in accreted and suspect' terrains; deposits formed at or near the sea floor or from hot springs; and those formed in successively deeper zones as magmatic deposits, vein to replacement deposits, skarns, and porphyries. Deposits within and directly linked to intrusive rocks (magmatic, porphyries, skarns), replacement deposits, possible manto deposits, deep to shallow veins and related deposits formed at the surface, volcanogenic massive sulphides and sedex deposits are then discussed. Sedimentary-hosted deposits of gypsum, barite, phosphate and other industrial minerals are not covered, nor are coal, uranium, pegmatite-hosted deposits, molybdenum prophyries or some of the less common deposit types such as carbonatites, tin greisens, and placers.