Fractal particle size distribution of pulverized fault rocks as a function of distance from the fault core-Reference-Cited by-同舟云学术

Fractal particle size distribution of pulverized fault rocks as a function of distance from the fault core

Published:2015-05-23 Issue:10 Volume:42 Page:3811-3819
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Muto Jun¹,Nakatani Tsurugi¹²,Nishikawa Osamu³,Nagahama Hiroyuki¹

Affiliation:

1. Department of Earth ScienceTohoku University Sendai Japan

2. Mitsubishi Materials Corporation, Higashitani Mine Kitakyushu City Japan

3. Faculty of International Resource SciencesAkita University Akita Japan

Funder

MEXT KAKENHI

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL064026

Reference44 articles.

1. Particle size distribution of cataclastic fault materials from Southern California: A 3-D study

2. Dynamic rupture on a material interface with spontaneous generation of plastic strain in the bulk

3. Cataclasis and processes of particle size reduction

4. 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 J. N.;Eos Trans. AGU,2001

5. Rupture mechanism and interface separation in foam rubber models of earthquakes: a possible solution to the heat flow paradox and the paradox of large overthrusts

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