Mid-Ocean Ridge Hydrothermal Fluxes and the Chemical Composition of the Ocean¶
Elderfield, & Schultz. (1996). Mid-Ocean Ridge Hydrothermal Fluxes and the Chemical Composition of the Ocean. Annual Review of Earth and Planetary Sciences.
Cited by¶
1 citation across 1 artifact.
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Domain-specific¶
- Hydrothermal Circulation
- Mid-ocean-ridge hydrothermal systems — the canonical case since the 1977 Galápagos Rift discovery: seawater descends into cracked basaltic crust, is heated by newly-emplaced igneous rock, and discharges through black-smoker and diffuse vents, with flux comparable to global riverine input
This sourceReview presenting established geophysical estimates of mid-ocean ridge axial heat fluxes and of the total hydrothermal flux, partitioned between high-temperature black smoker and lower-temperature diffuse flow.
Supported in partVerified against the work's full text
“Geophysical estimates of mid-ocean ridge axial heat fluxes (2–4 × 1012 W) and of the total hydrothermal flux (9 ± 2 × 1012 W) are well established.”
- Mid-ocean-ridge hydrothermal systems — the canonical case since the 1977 Galápagos Rift discovery: seawater descends into cracked basaltic crust, is heated by newly-emplaced igneous rock, and discharges through black-smoker and diffuse vents, with flux comparable to global riverine input
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