Mineralogical and chemical characteristics of hydrothermal alteration associated with the Proterozoic Vamp Lake Cu-Zn sulfide deposit, Flin Flon area
The Vamp Lake deposit is a stratiform, metamorphosed Cu-Zn massive sulfide deposit in the Proterozoic Flin Flon-Snow Lake greenstone belt of northern Manitoba. The deposit occurs at the contact between underlying mafic flows and overlying intermediate to felsic volcaniclastic rocks and flows in a 50...
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2012
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| Online Access: | http://hdl.handle.net/1993/7347 |