Endako molybdenite deposit and surrounding area were examined in detail, with particular attention to petrology and genesis of Topley Intrusions, regional structural setting and structural history of Endako orebody, sulphide and alteration mineralogy, fluid inclusion geothermometry of vein quartz, and minor element content of orebody pyrite. The host rock, Endako Quartz Monzonite, is a relatively early phase of Topley Intrusions that range in composition from diorite to granite, and in age from Middle Jurassic to Lower Cretaceous. Endako stockwork was localized by wrench faulting and doming generated by cooling of the batholith and intrusion of pre-mineral dykes. Hydrothermal fluids that altered and mineralized the stockwork were generated ...
The Mitchell-Sulphurets region is in the heart of the Coast Mountains of northwest British Columbia....
The Snip mine consists of an auriferous southwest-dipping shear vein system in a north-dipping Trias...
The Driftwood Property is located in the southwest corner of the McConnell Creek map-area, about 87 ...
Endako molybdenite deposit and surrounding area were examined in detail, with particular attention t...
Granitic rocks of the Topley intrusives underlying 100 square miles, centered around Endako, north ...
The Tuzo Creek Molybdenite Prospect is in southern British Columbia approximately twenty air-miles e...
Copper-silver mineralization at Sam Goosly occurs as a conformable lens within pyroclastic dacites o...
Two Mississippi Valley-type (MVT) ore deposits, Kicking Horse and Monarch, have been studied with th...
The Island Copper deposit at Port Hardy, approximately 200 miles northwest of Vancouver, B.C., consi...
Geology, opaque mineralogy, and alteration assemblages of the Sam Goosly copper-silver-antimony depo...
The Lorraine property area occupies the north eastern part of the Duckling Creek syenite located wit...
The Erickson mine is within the McDame lode gold camp, aproximately 12 km southeast of Cassiar, Brit...
Treasure Mountain is an epithermal style lead-zinc-silver deposit situated within the northern exten...
The Early Jurassic (>188-185 Ma) Turnagain ultramafic-mafic body, a composite Alaskan-type intrusion...
Detailed investigation of the Boss Mountain molybdenite deposits, which are on the northeast slope ...
The Mitchell-Sulphurets region is in the heart of the Coast Mountains of northwest British Columbia....
The Snip mine consists of an auriferous southwest-dipping shear vein system in a north-dipping Trias...
The Driftwood Property is located in the southwest corner of the McConnell Creek map-area, about 87 ...
Endako molybdenite deposit and surrounding area were examined in detail, with particular attention t...
Granitic rocks of the Topley intrusives underlying 100 square miles, centered around Endako, north ...
The Tuzo Creek Molybdenite Prospect is in southern British Columbia approximately twenty air-miles e...
Copper-silver mineralization at Sam Goosly occurs as a conformable lens within pyroclastic dacites o...
Two Mississippi Valley-type (MVT) ore deposits, Kicking Horse and Monarch, have been studied with th...
The Island Copper deposit at Port Hardy, approximately 200 miles northwest of Vancouver, B.C., consi...
Geology, opaque mineralogy, and alteration assemblages of the Sam Goosly copper-silver-antimony depo...
The Lorraine property area occupies the north eastern part of the Duckling Creek syenite located wit...
The Erickson mine is within the McDame lode gold camp, aproximately 12 km southeast of Cassiar, Brit...
Treasure Mountain is an epithermal style lead-zinc-silver deposit situated within the northern exten...
The Early Jurassic (>188-185 Ma) Turnagain ultramafic-mafic body, a composite Alaskan-type intrusion...
Detailed investigation of the Boss Mountain molybdenite deposits, which are on the northeast slope ...
The Mitchell-Sulphurets region is in the heart of the Coast Mountains of northwest British Columbia....
The Snip mine consists of an auriferous southwest-dipping shear vein system in a north-dipping Trias...
The Driftwood Property is located in the southwest corner of the McConnell Creek map-area, about 87 ...