Geoscientific studies on the Quaternary faulting and geomorphic processes of the Ryukyu arc, southwestern Japan
Author:
Affiliation:
1. Faculty of Education, University of the Ryukyus
2. Research Institute of Earthquake and Volcano Geology, Geological Survey of Japan, AIST
Publisher
Japan Association for Quaternary Research
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
https://www.jstage.jst.go.jp/article/jaqua/58/6/58_377/_pdf
Reference47 articles.
1. Angelier, J. (1984) Tectonic analysis of fault slip data sets. Journal of Geophysical Research, 89, 5835-5848.
2. Arai, K., Inoue, T., Ikehara, K. and Sasaki, T. (2014) Episodic subsidence and active deformation of the forearc slope along the Japan Trench near the epicenter of the 2011 Tohoku Earthquake. Earth and Planetary Science Letters, 408, 9-15.
3. Bense, V.F., Gleeson, T., Loveless, S.E., Bour, O. and Scibek, J. (2013) Fault zone hydrogeology. Earth-Science Reviews, 127, 171-192.
4. Billi, A., Salvini, F. and Storti, F. (2003) The damage zone-fault core transition in carbonate rocks : implications for fault growth, structure and permeability. Journal of Structural Geology, 25, 1779-1794.
5. Caine, J.S., Evans, J.P. and Forster, C.B. (1996) Fault zone architecture and permeability structure. Geology, 24, 1025-1028.
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1. Neotectonics in Ryukyu arc－Future works on processes of uplift and subsidence－;The Journal of the Geological Society of Japan;2024
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