Isostasy and the ambient state of stress in the oceanic lithosphere-Reference-Cited by-同舟云学术

Isostasy and the ambient state of stress in the oceanic lithosphere

Published:1981-09-10 Issue:B9 Volume:86 Page:7801-7807
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res.

Author:

Dahlen F. A.

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/v086/iB09/JB086iB09p07801/JB086iB09p07801.pdf

Reference36 articles.

1. Stresses in the lithosphere caused by crustal thickness inhomogeneities;Artyushkov;J. Geophys. Res.,1973

2. Can the earth's crust be in a state of isostasy?;Artyushkov;J. Geophys. Res.,1974

3. Oceanic intraplate earthquakes: Implications for local and regional intraplate stress;Bergman;J. Geophys. Res.,1980

4. Earthquakes and bending of plates at trenches;Chapple;J. Geophys. Res.,1979

5. Evaluation of the forces that drive the plates;Chapple;J. Geophys. Res.,1977

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