Fluid inclusion constraints on the origin of the brines responsible for Pb–Zn mineralization at Pine Point and coarse non-saddle and saddle dolomite formation in southern Northwest Territories
The Pine Point region is a classic metallogenic mining camp that produced over 58 million short tons of Zn-Pb ore from approximately 40 base-metal mineralized deposits hosted by Middle Devonian carbonates. The ore deposits are localized in paleokarstic features found in the epigenetic 'Presqu&#...
| Published in: | Geofluids |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
2007
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| Subjects: | |
| Online Access: | https://gfzpublic.gfz-potsdam.de/pubman/item/item_1943891 |