Constraints on hydrothermal heat flux through the oceanic lithosphere from global heat flow¶
Stein. (1994). Constraints on hydrothermal heat flux through the oceanic lithosphere from global heat flow. Journal of Geophysical Research: Solid Earth.
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Domain-specific¶
- Hydrothermal Circulation
- . Volcanic-arc and continental geothermal systems — Yellowstone, Iceland, New Zealand, and the East African Rift as surface manifestations driven by shallow magma chambers and elevated crustal heat flux. Ore-deposit formation — hydrothermal fluids as the transport machinery concentrating dispersed metals into economic deposits: porphyry copper, volcanogenic massive sulfide, epithermal gold, Mississippi Valley-type lead-zinc, skarn. Sedimentary-basin diagenesis and petroleum geology — deep-basin hydrothermal circulation altering sediments and participating in petroleum migration and maturation. Origin-of-life and astrobiology — alkaline-vent systems (Russell–Martin hypothesis) as candidate cradles for the emergence of life on early Earth and on icy moons (Europa, Enceladus). Crustal heat budget and global geochemistry — the hydrothermal flux carrying a substantial fraction of oceanic-crust heat flow and mediating ocean chemistry (Mg removal, alkali-metal exchange, isotope fractionation) at globally significant rates
This sourceReview estimating that 34% (11e12 W) of the predicted global oceanic heat flux of 32e12 W occurs by hydrothermal flow, estimates held to bear on the chemistry of the oceans.
Supported in partVerified against the publisher's abstract
“We estimate that of the predicted global oceanic heat flux of 32×1012 W, 34% (11×1012 W) occurs by hydrothermal flow.”
- . Volcanic-arc and continental geothermal systems — Yellowstone, Iceland, New Zealand, and the East African Rift as surface manifestations driven by shallow magma chambers and elevated crustal heat flux. Ore-deposit formation — hydrothermal fluids as the transport machinery concentrating dispersed metals into economic deposits: porphyry copper, volcanogenic massive sulfide, epithermal gold, Mississippi Valley-type lead-zinc, skarn. Sedimentary-basin diagenesis and petroleum geology — deep-basin hydrothermal circulation altering sediments and participating in petroleum migration and maturation. Origin-of-life and astrobiology — alkaline-vent systems (Russell–Martin hypothesis) as candidate cradles for the emergence of life on early Earth and on icy moons (Europa, Enceladus). Crustal heat budget and global geochemistry — the hydrothermal flux carrying a substantial fraction of oceanic-crust heat flow and mediating ocean chemistry (Mg removal, alkali-metal exchange, isotope fractionation) at globally significant rates
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