Insights into pulverized rock formation from dynamic rupture models of earthquakes

Author:

Payne R.M.,Duan B.

Funder

NSF

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference27 articles.

1. Dynamic fracturing by successive coseismic loadings leads to pulverization in active fault zones;Aben;J. geophys. Res.,2016

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

3. Brune J.N. AGU Fall Meeting Abstracts. 2001. Fault-normal dynamic unloading and loading: an explanation for “non-gouge” rock powder and lack of fault-parallel shear bans along the San Andreas Fault. Abstract S22B-0655.

4. Slip distribution of the 1992 Landers earthquake and its implications for earthquake source mechanics;Cohee;Bull. seism. Soc. Am.,1994

5. Three-dimensional simulation of spontaneous rupture: the effect of nonuniform prestress;Day;Bull. seism. Soc. Am.,1982

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