地中レーダ探査からみた丹那断層田代地点の極浅部地下の左横ずれ変形構造
Author:
Affiliation:
1. Central Research Institute of Electric Power Industry
2. Faculty of Science and Engineering, Doshisha University
3. Pasco Corporation
4. Museum of Natural and Environmental History, Shizuoka
Publisher
Japan Association for Quaternary Research
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
https://www.jstage.jst.go.jp/article/jaqua/advpub/0/advpub_62.2207/_pdf
Reference20 articles.
1. 物理探査学会編（2016）物理探査ハンドブック 増補改訂版．1045 p，物理探査学会．
2. Daniels, D.J. ed. (1996) Surface-penetrating radar. 300 p, The Institute of Electrical Engineers.
3. Gross, R., Gree, A.G. and Horstmeyer, H. (2004) Location and geometry of the Wellington Fault (New Zealand) defined by detailed three-dimensional georadar data. Journal of Geophysical Research, 109, B05401, doi: 10.1029/2003JB002615.
4. Hall, N.T., Wright, R.H. and Clahan, K.B. (1999) Paleoseismic studies of the San Francisco Peninsula segment of the San Andreas fault zone near Woodside, California. Journal of Geophysical Research, 104, 23,215-23,236.
5. 伊原敬之助・石井清彦（1932）北伊豆震災地調査報文．地質調査報告112，111 p，地質調査所．
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1. Preface of the Special Issue “Environmental Change and Mega Disasters Unraveled from Terrestrial Archives: Toward Disaster Prevention and Mitigation”;The Quaternary Research (Daiyonki-Kenkyu);2024-05-01
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