Distribution and characteristics of landslides induced by the Iwate–Miyagi Nairiku Earthquake in 2008 in Tohoku District, Northeast Japan

Author:

Yagi Hiroshi,Sato Go,Higaki Daisuke,Yamamoto Miki,Yamasaki Takanari

Publisher

Springer Science and Business Media LLC

Subject

Geotechnical Engineering and Engineering Geology

Reference14 articles.

1. Horikawa H (2008) Source process of the Iwate–Miyagi Nairiku Earthquake in 2008 inferred from strong motion wave forms. AFRC News 81(7):1–4

2. Japan Meteorological Agency (2008) Evaluation of the Iwate–Miyagi Nairiku Earthquake in 2008 (mainly on surface rupture). http://www.jishin.go.jp/main/chousa/08jul_iwate_miyagi/p07.htm

3. Joint Observation Group of Universities and Research Institute across the Country (2008) Feature: Iwate–Miyagi Nairiku Earthquake 2008. http://www.aob.geophys.tohoku.ac.jp/GIMNE2008/

4. National Research Institute for Earth Science and Disaster Prevention (2008) Peak acceleration contour map, http://www.kyoshin.bosai.go.jp/kyoshin/

5. Nunohara K, Yoshida T, Yoshida R (2008) Relationship between earthquake disasters and caldera structures using of GIS. Abstract, the 2009 National Conference, Geological Society of Japan, http://www.geosociety.jp/hazard/content0035.html

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