SEAFLOOR HYDROTHERMAL ACTIVITY¶
Von Damm. (1990). SEAFLOOR HYDROTHERMAL ACTIVITY: BLACK SMOKER CHEMISTRY AND CHIMNEYS.
Cited by¶
1 citation across 1 artifact.
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Domain-specific¶
- Hydrothermal Circulation
- That rock-fluid chemical exchange is what distinguishes hydrothermal circulation from pure thermal convection: descending seawater loses magnesium and sulfate to the basalt; ascending fluid gains iron, manganese, copper, zinc, hydrogen sulfide, and helium-3, emerging at black-smoker vents at temperatures up to 400 °C or at lower-temperature diffuse seeps
This sourceReview of seafloor hydrothermal venting, first discovered in 1977 at the Galapagos spreading centre, reporting vent temperatures from just above ambient (~24 C) to ~350 C and common chemical characteristics among the fluids.
Supported in partVerified against the publisher's abstract
“Venting of hydrothermal solutions on the seafloor, first discovered in 1977 at the Galapagos spreading center”
- That rock-fluid chemical exchange is what distinguishes hydrothermal circulation from pure thermal convection: descending seawater loses magnesium and sulfate to the basalt; ascending fluid gains iron, manganese, copper, zinc, hydrogen sulfide, and helium-3, emerging at black-smoker vents at temperatures up to 400 °C or at lower-temperature diffuse seeps
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Registry ID ref:bb54d7198b4a · see in the full table