Terminal basin as a target for turbidite paleoseismology
Author:
Affiliation:
1. Institute of Geology and Geoinformation, Geological Survey of Japan
Publisher
Japan Association for Quaternary Research
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
https://www.jstage.jst.go.jp/article/jaqua/54/6/54_345/_pdf
Reference55 articles.
1. Adams, J. (1990) Paleoseismicity of the Cascadia subduction zone : Evidence from turbidites off the Oregon-Washington margin. Tectonics, 9, 569-583.
2. Arai, K., Naruse, H., Miura, R., Kawamura, K., Hino, R., Ito, Y., Inazu, D., Yokokawa, M., Izumi, N., Murayama, M. and Kasaya, T. (2013) Tsunami-generated turbidity current of the 2011 Tohoku-oki earthquake. Geology, 41, 1195-1198.
3. Araoka, D., Yokoyama, Y., Suzuki, A., Goto, K., Miyagi, K., Miyazawa, K., Matsuzaki, H. and Kawahata, H. (2013) Tsunami recurrence revealed by Porites coral boulders in the southern Ryukyu Islands, Japan. Geology, 41, 919-922.
4. Ashi, J., Ikehara, K., Kinoshita, M. and KY04-11, KH-10-3 shipboard scientists (2012) Settling of earthquake-induced turbidity on the accretionary prism slope of the central Nankai subduction zone. Yamada, Y., Kawamura, K., Ikehara, K., Ogawa, Y., Urgeles, R., Mosher, D., Chaytor, J. and Strasser, M. (eds.) Submarine mass movements and their consequences, Advances in natural and technological hazards research, 31, Springer, 561-571.
5. Ashi, J., Sawada, R., Omura, A. and Ikehara, K. (2014) Accumulation of an earthquake-induced extremely turbid layer in a terminal basin of the Nankai accretionary prism. Earth, Planets and Space, 66, 51, doi : 10.1186/1880-5981-66-51.
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