Borehole observatories record driving forces for hydrotheraial circulation in young oceanic crust

Author:

Davis Earl,Becker Keir

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences

Reference10 articles.

1. Formation temperatures and pressures in a sedimented rift hydrothermal system: Ten months of CORK observations, Holes 857D and 858G;Davis;Proc. Ocean Drill. Program Sci. Results,1994

2. CORK: A hydrologic seal and downhole observatory for deep ocean boreholes;Davis;Proc. Ocean Drill. Program Initial Rep.,1992

3. An unequivocal case for high Nusselt number hydrothermal convection in sediment-buried igneous oceanic crust;Davis;Earth Planet. Sci. Lett.,1997

4. Correlation between seafloor heat flow and basement relief: Observational and numerical examples and implications for upper crustal permeability;Fisher;J. Geophys. Res.,1995

5. The permeability of young oceanic crust east of Juan de Fuca Ridge, as determined using borehole thermal measurements;Fisher;Geophys. Res. Lett.,1997

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