Origin of pulverized rocks during earthquake fault rupture

Author:

Yuan Fuping,Prakash Vikas,Tullis Terry

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

Reference62 articles.

1. The damage mechanics of brittle solids in compression;Ashby;Pure Appl. Geophys.,1990

2. Dynamic ruptures in recent models of earthquake faults;Ben-Zion;J. Mech. Phys. Solids,2001

3. Dynamic rupture on a material interface with spontaneous generation of plastic strain in the bulk;Ben-Zion;Earth Planet. Sci. Lett.,2005

4. Reply to comment on “How fast is rupture during an earthquake? New insights from the 1999 Turkey earthquakes,”;Bouchon;Geophys. Res. Lett.,2002

5. Fault-normal dynamic loading and unloading: An explanation for “nongouge” rock powder and lack of fault-parallel shear bands along the San Andreas Fault;Brune;Eos Trans. AGU,2001

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