Projects
Doubleview Gold Corp is focused on the exploration and development of high-value critical metals essential for global industries. Our flagship Hat Project, located in British Columbia’s Golden Triangle, has the potential to be a major source of copper, scandium, cobalt, gold, and silver. With a commitment to innovation, and responsible resource expansion, we are advancing projects that it may contribute to the future of clean energy, technology, and industrial growth.
Hat Copper-Gold
Hat is located 50 km northwest of Telegraph Creek north-western BC. Situated in the Stikine District that includes the large Galore Creek, Schaft Creek, Red Chris, and Kutcho copper deposits that collectively have 7.65M tonnes copper, 14.9 M oz gold and 148.5 M oz silver in measured and indicated resources.
Geology
Situated within the Stikinia terrane at the western edge of the intermontane physiographic province, proximal to the Coast Crystalline Belt. The “Stikinia” which has similar characteristics but is less explored than the “Quesnellia” terrane (a north-trending belt of intermediate volcaniclastic rocks that extends northerly through the length of the province), is host to several active mines and numerous properties that are either awaiting development or re-activation. In both terranes most deposits are closely related to dioritic and granodioritic plutons of Early- to Mid-Jurassic age.
Property formations are members of the Stuhini Group of island arc-related andesitic to basaltic volcanic rocks and derived clastic sedimentary rocks of Upper Triassic age, and small intrusive bodies of dioritic and gabbroic composition. Structural alignment of both formations and intrusions is north-westerly.
Red Spring Copper Gold Silver & Zinc Project
Red Spring project is located in central interior British Columbia, Canada, 100 km northeast of Hazelton, B. C. Copper mineralization on the Red Spring property was discovered by Canadian Superior Exploration Ltd. in 1972.
Exploration in 1972 by C.S.E. included geological, geochemical and geophysical surveys and 2,972 feet of drill testing. Additional drilling (3 drill holes, 1156 ft.) was completed in 1976 by City Services Mineral Corp. The historic drill cores may be located on the property.
IN 1990, a very preliminary metallurgical test work on a drill core sample with an indicated grade of 0.70% copper showed that a concentrate grading 24.4% copper, 7.99 g/t gold and 1043 g/t silver could be achieved with 78.9% recovery of copper, 79.0% of gold and 81.4%of silver. The laboratory suggested that recoveries could be improved.
The property is underlain by Jurassic age Hazelton Group volcanics and volcanoclastic sediments. The geologic model suggests that a copper-rich layer of dolomitic limestone, centrally located on the property, carries disseminated chalcopyrite with associated silver and gold values.
Doubleview has conducted several surveys including geochemical sampling and airborne VTEM.
The Red Spring property is located in the asserted traditional 27,250 square kilometre territory of the Takla First Nation. The territory is a rich environment of lakes, rivers, forests and mountains between the Skeena Mountains to the west and the Rocky Mountains to the east.
Several past-producing mines have operated in the territory including the Shasta (AU, AG, ZN, CU, PB), Baker (AU, AG, CU, ZN, PB), and Kemess South (CU, AU, MO, AG) mines. The McConnell Creek (AU, PT) placer mining area lies east of the Red Spring property.
