Origin of elevated sediment permeability in a hydrothermal seepage zone, eastern flank of the Juan de Fuca Ridge, and implications for transport of fluid and heat
- 10 January 2000
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 105 (B1) , 913-928
- https://doi.org/10.1029/1999jb900360
Abstract
No abstract availableKeywords
This publication has 66 references indexed in Scilit:
- The permeability of young oceanic crust east of Juan de Fuca Ridge Determined using borehole thermal measurementsGeophysical Research Letters, 1997
- An unequivocal case for high Nusselt number hydrothermal convection in sediment-buried igneous oceanic crustEarth and Planetary Science Letters, 1997
- Correlation between seafloor heat flow and basement relief: Observational and numerical examples and implications for upper crustal permeabilityJournal of Geophysical Research, 1995
- Seafloor hydrothermal systemsJournal of Geophysical Research, 1995
- Comparison of plate and asthenospheric flow models for the thermal evolution of oceanic lithosphereGeophysical Research Letters, 1994
- Ecology of deep‐sea hydrothermal vent communities: A reviewReviews of Geophysics, 1993
- Impact of crustal evolution on changes of the seismic properties of the uppermost ocean crustReviews of Geophysics, 1992
- Correlated sediment thickness, temperature gradient and excess pore pressure in a marine fault block basinGeophysical Research Letters, 1984
- The heat flow through oceanic and continental crust and the heat loss of the EarthReviews of Geophysics, 1980
- Hydrothermal convection at slow-spreading mid-ocean ridgesTectonophysics, 1979