Evolution of Fault Zones and Its Rheology-Reference-Cited by-同舟云学术

Evolution of Fault Zones and Its Rheology

Published:2020-08-25 Issue:4 Volume:129 Page:473-489
ISSN:0022-135X
Container-title:Journal of Geography (Chigaku Zasshi)
language:en
Short-container-title:Journal of Geography(Chigaku Zasshi)

Author:

OOHASHI Kiyokazu¹^ORCID,TAKESHITA Toru²,HIRAUCHI Ken-ichi³

Affiliation:

1. Graduate School of Sciences and Technology for Innovation, Yamaguchi University

2. Graduate School of Science, Hokkaido University

3. Department of Geoscience, Faculty of Science, Shizuoka University

Publisher

Tokyo Geographical Society

Subject

Materials Chemistry

Link

https://www.jstage.jst.go.jp/article/jgeography/129/4/129_129.473/_pdf

Reference108 articles.

1. Anderson, J.G., Wesnousky, S.G. and Stirling, M.W. (1996): Earthquake size as a function of fault slip rate. Bulletin of the Seismological Society of America, 86, 683-690.

2. Barth, N.C., Boulton, C., Carpenter, B.M., Batt, G.E. and Toy, V.G. (2013): Slip localization on the southern Alpine Fault, New Zealand. Tectonics, 32, 620-640.

3. Bird, P. (1984): Hydration-phase diagrams and friction of montmorillonite under laboratory and geologic conditions, with implications for shale compaction, slope stability, and strength of fault gouge. Tectonophysics, 107, 235-260.

4. Bos, B. and Spiers, C.J. (2002): Frictional-viscous flow ofphyllosilicate-bearing fault rocks: microphysical model and implications for crustal strength profiles. Journal of Geophysical Research, 107, 1-13.

5. Boulton, C., Moore, D.E., Lockner, D.A., Toy, V.G., Townend, J. and Sutherland, R. (2014): Frictional properties of exhumed fault gouges in DFDP-1 cores, Alpine Fault, New Zealand. Geophysical Research Letter, 41, 356-362.

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