Deep crustal geothermal measurements, hole 504B, Costa Rica Rift

Author:

Becker Keir,Langseth M. G.,Von Herzen R. P.,Anderson R. N.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference46 articles.

1. The relation between heat flow, sediment thickness, and age in the eastern Pacific;Anderson;J. Geophys. Res.,1976

2. Permeability, underpressures, and convection in the oceanic crust near the Costa Rica Rift, eastern equatorial Pacific;Anderson;J. Geophys. Res.,1982

3. The mechanisms of heat transfer through the floor of the Indian Ocean;Anderson;J. Geophys. Res.,1977

4. DSDP hole 504B, the first reference section over 1 km through layer 2 of the oceanic crust;Anderson;Nature,1982

5. In situ permeability variation in the upper kilometer of the oceanic crust of the Costa Rica Rift (abstract);Anderson;Eos Trans. AGU,1982

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