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December 01, 1993
Mineralogy and geochemistry of active and inactive chimneys and massive sulfide, Middle Valley, northern Juan de Fuca Ridge; an evolving hydrothermal system
D. E. Ames
;
D. E. Ames
Geological Survey of Canada, Ottawa, ON, Canada
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The Canadian Mineralogist (1993) 31 (4): 997–1024.
Article history
first online:
02 Mar 2017
Citation
D. E. Ames, J. M. Franklin, M. D. Hannington; Mineralogy and geochemistry of active and inactive chimneys and massive sulfide, Middle Valley, northern Juan de Fuca Ridge; an evolving hydrothermal system. The Canadian Mineralogist 1993;; 31 (4): 997–1024. doi:
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Index Terms/Descriptors
- anhydrite
- base metals
- East Pacific
- electron probe data
- hematite
- hydrothermal alteration
- hydrothermal processes
- hydrothermal vents
- iron ores
- Juan de Fuca Ridge
- lead-zinc deposits
- magnetite
- massive deposits
- metal ores
- metasomatism
- mid-ocean ridges
- Middle Valley
- mineralization
- North Pacific
- Northeast Pacific
- ocean floors
- oxides
- Pacific Ocean
- sulfates
- sulfides
- Ben Hill Deposit
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