Fluid Inclusion Study of Vein Minerals from the Si1,ver Queen Mine, Central British Columbia (!93l/2!)
نویسنده
چکیده
Silver Queen mint in central British Columbia, is located approximately 35 kilometres south of Houston and 3 kilometres east of 0wt.n Lake (Figure 2-7-1). Although currently inactive, it was worked briefly in the early 1970s for gold. silver, copper, zinc, lead and cadmium. The deposit is hosted by Cretaceous rocks of the informal Tip Top Hill group (78.322.67 Ma, K-Ar whole rock), with the age of mineralization bracketed by pre and post-mineralization
منابع مشابه
Syn-hydrothermal Development of Fractures in the Silver Queen Mine Area, Owen Lake,, Central British Columbia* (93l/2)
The site and character of precious and basemetal epithermal deposits is determined by several principal factors which include: structure, stratigraphy, lithology, pressure and temperature. hydrology, chemistry of the mineralizing fluid, and syn-hydrothermal development of permeability or changes in hydraulic gradient (White and Hedenquist, 1990). This study investigates the syn-hydrothermal dev...
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