Viscoelastic stress relaxation on deep fault sections as a possible source of very long period elastic waves

Author:

Bonafede M.,Boschi E.,Dragoni M.

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

Reference73 articles.

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2. Micromechanisms of flow and fracture and their relevance to the theology of the upper mantle;Ashby;Philos. Trans. R. Soc. London, Ser. A,1977

3. Source mechanism from spectra of long period surface waves;Ben-Menahem;J. Geophys. Res.,1963

4. Dislocations and the theory of fracture;Bilby,1968

5. Thermal and mechanical models of continent-continent convergence zones;Bird;J. Geophys. Res.,1975

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