Depth-dependent stress field in and around the Atotsugawa fault, central Japan, deduced from microearthquake focal mechanisms: Evidence for localized aseismic deformation in the downward extension of the fault-Reference-Cited by-同舟云学术

Depth-dependent stress field in and around the Atotsugawa fault, central Japan, deduced from microearthquake focal mechanisms: Evidence for localized aseismic deformation in the downward extension of the fault

Published:2011-01-21 Issue:B1 Volume:116 Page:
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Imanishi Kazutoshi,Kuwahara Yasuto,Takeda Tetsuya,Mizuno Takashi,Ito Hisao,Ito Kiyoshi,Wada Hiroo,Haryu Yoshikatsu

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/jb1101/2010JB007900/2010JB007900.pdf

Reference81 articles.

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4. Mapping stress and structurally controlled crustal shear velocity anisotropy in California;Boness;Geology,2006

5. Friction of rocks;Byerlee;Pure Appl. Geophys.,1978

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