Mineral assemblage anomalies in the slip zone of the 1999 Taiwan Chi-Chi earthquake: Ultrafine particles preserved only in the latest slip zone-Reference-Cited by-同舟云学术

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Mineral assemblage anomalies in the slip zone of the 1999 Taiwan Chi-Chi earthquake: Ultrafine particles preserved only in the latest slip zone

Published:2014-05-01 Issue:9 Volume:41 Page:3052-3059
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Hirono Tetsuro¹,Kameda Jun²,Kanda Hiroki¹,Tanikawa Wataru³,Ishikawa Tsuyoshi³

Affiliation:

1. Department of Earth and Space Science, Graduate School of Science; Osaka University; Toyonaka Osaka Japan

2. Department of Earth Sciences, School of Science; Hokkaido University; Sapporo Japan

3. Kochi Institute for Core Sample Research; Japan Agency for Marine-Earth Science and Technology; Nankoku Kochi Japan

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference34 articles.

1. Mineralogy and sedimentation of recent deep-sea clays in the Atlantic Ocean and adjacent seas and oceans;Biscaye;Geol. Soc. Am. Bull.,1965

2. Thermochemical pressurization of faults during coseismic slip;Brantut;J. Geophys. Res.,2010

3. High-velocity frictional properties of a claybearing fault gouge and implications for earthquake mechanics;Brantut;J. Geophys. Res.,2008

4. Fracture surface energy of the Punchbowl fault, San Andreas system;Chester;Nature,2005

5. An earthquake slip zone is a magnetic recorder;Chou;Geology,2012

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