Origin of carbonate hosted gold rich replacement deposits and related mineralization styles in the Ketza River deposit, Yukon Territory
The Ketza River deposit consists of gold-rich, base metal-poor oxidized and unoxidized manto style orebodies and Fe-silicate alteration zones hosted in Early Cambrian limestones, and quartzsulphide veins and stockwork in Late Proterozoic to Eady Cambrian metasedimentary rocks. Sulphide mineralogy...
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| Format: | Others |
| Language: | English |
| Published: |
2009
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| Online Access: | http://hdl.handle.net/2429/8406 |