Regional heat flow variations across the sedimented Juan de Fuca Ridge eastern flank: Constraints on lithospheric cooling and lateral hydrothermal heat transport-Reference-Cited by-同舟云学术

Regional heat flow variations across the sedimented Juan de Fuca Ridge eastern flank: Constraints on lithospheric cooling and lateral hydrothermal heat transport

Published:1999-08-10 Issue:B8 Volume:104 Page:17675-17688
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res.

Author:

Davis E. E.,Chapman D. S.,Wang K.,Villinger H.,Fisher A. T.,Robinson S. W.,Grigel J.,Pribnow D.,Stein J.,Becker K.

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

Link

http://www.agu.org/journals/jb/v104/iB08/1999JB900124/1999JB900124.pdf

Reference37 articles.

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2. Permeability measurements in Hole 896A and implications for the lateral variability of upper crustal permeability at Sites 504 and 896;Becker;Proc. Ocean Drill. Program Sci. Results,1996

3. Problems with imaging cellular hydrothermal convection in oceanic crust;Davis;Geophys. Res. Lett.,1996

4. Heat flow measured over the Juan de Fuca Ridge: Evidence for widespread hydrothermal circulation in a highly heat transportive crust;Davis;J. Geophys. Res.,1977

5. Heat-flow variations correlated with buried basement topography on the Juan de Fuca Ridge flank;Davis;Nature,1989

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