Geology, mineralogy, and chemistry of sediment-hosted clastic massive sulfides in shallow cores, Middle Valley, northern Juan de Fuca Ridge
Journal Article
·
· Economic Geology (plus the Bulletin of the Society of Economic Geologists); (United States)
- Geological Survey of Canada, Ottawa, Ontario (Canada)
Middle Valley is a sediment-covered rift near the northern end of Juan de Fuca Ridge. Hydrothermal fluids are presently being discharged at two vent fields about 3 km apart, Bent Hill and the area of active venting. The hydrothermally active chimneys at both Bent Hill and the area of active venting consist of anhydrite and Mg-rich silicates with minor pyrite, Cu-Fe sulfide, sphalerite, and galena. Hydrothermal discharge in these areas appears to be focused along extensional faults. At the Bent Hill massive sulfide deposit, clastic sulfide layers are interbedded with hydrothermally altered and unaltered hemipelagic and turbiditic sediment along the flanks of the sulfide mound. Sulfide textures and mineralogy suggest that the Bent Hill sulfide mound formed by the build-up and collapse of sulfide chimneys, the resedimentation of sulfide debris and the formation of clastic sulfide layers, and the infilling and replacement of clastic sulfides by hydrothermal fluids near vents. Sulfur isotope values that are consistently more positive than basaltic sulfur support the addition of seawater sulfur. Pb isotope values for the Bent Hill deposit that are transitional between midocean ridge basalt (MORB) and Middle Valley sediments indicate that the sulfides probably formed from fluids which originated in the oceanic crust but which have been modified by reaction with lower temperature (<274 C) fluids generated in the sedimentary pile, similar to those now venting in Middle Valley.
- OSTI ID:
- 7049377
- Journal Information:
- Economic Geology (plus the Bulletin of the Society of Economic Geologists); (United States), Journal Name: Economic Geology (plus the Bulletin of the Society of Economic Geologists); (United States) Vol. 88:8; ISSN 0361-0128; ISSN ECGLAL
- Country of Publication:
- United States
- Language:
- English
Similar Records
Southern Juan De Fuca Ridge and Escanaba Trough, Gorda Ridge: Comparison of hydrothermal deposits in sediment-free and sediment-covered ridge settings
Space-time relations of hydrothermal sulfide-sulfate-silica deposits at the northern Cleft Segment, Juan de Fuca Ridge
Stable isotope studies of vent fluids and chimney minerals, southern Juan de Fuca Ridge: Sodium metasomatism and seawater sulfate reduction
Conference
·
Fri Jun 01 00:00:00 EDT 1990
· AAPG Bulletin (American Association of Petroleum Geologists); (USA)
·
OSTI ID:6317651
Space-time relations of hydrothermal sulfide-sulfate-silica deposits at the northern Cleft Segment, Juan de Fuca Ridge
Conference
·
Wed Mar 31 23:00:00 EST 1993
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:5067396
Stable isotope studies of vent fluids and chimney minerals, southern Juan de Fuca Ridge: Sodium metasomatism and seawater sulfate reduction
Journal Article
·
Sat Oct 10 00:00:00 EDT 1987
· J. Geophys. Res.; (United States)
·
OSTI ID:5537010
Related Subjects
15 GEOTHERMAL ENERGY
150200 -- Geology & Hydrology of Geothermal Systems
152003* -- Geothermal Data & Theory-- Rock-Water-Gas Interactions
58 GEOSCIENCES
580000 -- Geosciences
CHEMISTRY
DEVELOPED COUNTRIES
FUMAROLES
GEOCHEMISTRY
GEOLOGIC DEPOSITS
GEOLOGIC STRUCTURES
GEOLOGY
HYDROTHERMAL ALTERATION
MINERALOGY
MINERALS
NORTH AMERICA
PACIFIC OCEAN
RIFT ZONES
SEAS
SEDIMENTS
SULFIDE MINERALS
SURFACE WATERS
USA
WASHINGTON
150200 -- Geology & Hydrology of Geothermal Systems
152003* -- Geothermal Data & Theory-- Rock-Water-Gas Interactions
58 GEOSCIENCES
580000 -- Geosciences
CHEMISTRY
DEVELOPED COUNTRIES
FUMAROLES
GEOCHEMISTRY
GEOLOGIC DEPOSITS
GEOLOGIC STRUCTURES
GEOLOGY
HYDROTHERMAL ALTERATION
MINERALOGY
MINERALS
NORTH AMERICA
PACIFIC OCEAN
RIFT ZONES
SEAS
SEDIMENTS
SULFIDE MINERALS
SURFACE WATERS
USA
WASHINGTON