The huge shallow slip during the 2011 Tohoku-Oki earthquake as a result of very low coseismic shear strength of the plate-boundary thrust material (R14-O-13)(abs.)

Geological Literature Search (GEOLIS) (Geological Survey of Japan / AIST)

The huge shallow slip during the 2011 Tohoku-Oki earthquake as a result of very low coseismic shear strength of the plate-boundary thrust material (R14-O-13)(abs.)

Authors=UJIIE Kohtaro, TANAKA Hanae, SAITO Tsubasa, TSUTSUMI Akito, MORI James J., KAMEDA Jun, CHESTER Frederick M., EGUCHI Nobuhisa, TOCZKO Sean, IODP Expedition343 scientists

Journal/Book_names=Abstracts, the 120th Annual Meeting of the Geological Society of Japan

volume=120

pages=115-115

Publish_year=2013

Publish_Country=JPN

Publisher=Geological Society of Japan

Language_of_Text=JA

ISSN=13483935

DOI=10.14863/geosocabst.2013.0_225

ID=201310679

@id=https://gbank.gsj.jp/ld/resource/geolis/201310679