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J-GLOBAL ID:201802280248436223   Reference number:18A1886910

Architecture of onshore fault zones

陸域断層の内部構造
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Volume: 124  Issue:Page: 759-775  Publication year: Sep. 15, 2018 
JST Material Number: F0528A  ISSN: 0016-7630  CODEN: CHTZA5  Document type: Article
Article type: 文献レビュー  Country of issue: Japan (JPN)  Language: JAPANESE (JA)
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Geological structure and tectonics 
Reference (153):
  • 相澤泰隆・小林健太・梅津健吾・山本 亮(Aizawa, Y., Kobayashi, K., Umetsu, K., and Yamamoto, R.), 2005, 2000年鳥取県西部地震の余震域およびその周辺に分布する断層岩類(Fault rocks in the aftershock area and the neighborhood of 2000 Tottori-ken Seibu earthquake).地質雑(Jour. Geol. Soc. Japan), 111, 737-750.
  • Ampuero, J. P. and Ben-Zion, Y., 2008, Cracks, pulses and macroscopic asymmetry of dynamic rupture on a bimaterial interface with velocity-weakening friction. Geophys. Jour. Int., 173, 674-692.
  • Andersen, T. B. and Austrheim, H., 2006, Fossil earthquakes recorded by pseudotachylytes in natural peridotite from the Alpine subduction complex of Corsica. Earth Planet. Sci. Lett., 343, 58-72.
  • Austrheim, H. and Boundy, T. M., 1994, Pseudotachylytes generated during seismic faulting and eclogitization of the deep crust. Science, 265, 82-83.
  • Behr, W. M. and Platt, J. P., 2011, A naturally constrained stress profile through the middle crust in an extensional terrane. Earth Planet. Sci. Lett., 303, 181-192.
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