Pore fluid advection and reaction in sediments of the eastern flank, Juan de Fuca Ridge, 48°N
- 1 April 2001
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 187 (1-2) , 173-189
- https://doi.org/10.1016/s0012-821x(01)00287-4
Abstract
No abstract availableKeywords
This publication has 41 references indexed in Scilit:
- Mid-Ocean Ridge Hydrothermal Fluxes and the Chemical Composition of the OceanAnnual Review of Earth and Planetary Sciences, 1996
- Hydrothermal circulation through mid-ocean ridge flanks: Fluxes of heat and magnesiumGeochimica et Cosmochimica Acta, 1994
- Constraints on hydrothermal heat flux through the oceanic lithosphere from global heat flowJournal of Geophysical Research, 1994
- Fluid flow in deep-sea carbonates: estimates based on porewater SrEarth and Planetary Science Letters, 1993
- FlankFlux: an experiment to study the nature of hydrothermal circulation in young oceanic crustCanadian Journal of Earth Sciences, 1992
- Large-scale lateral advection of seawater through oceanic crust in the central equatorial PacificEarth and Planetary Science Letters, 1991
- Heat-flow variations correlated with buried basement topography on the Juan de Fuca Ridge flankNature, 1989
- Pore water chemistry of the Mounds Hydrothermal Field, Galapagos Spreading Center: Results from Glomar Challenger Piston CoringJournal of Geophysical Research, 1983
- Upwelling of Hydrothermal Solutions Through Ridge Flank Sediments Shown by Pore Water ProfilesScience, 1982
- Deep-tow observations at the mounds abyssal hydrothermal field, Galapagos RiftEarth and Planetary Science Letters, 1977