Shinseiko-landslide induced by the great Kanto Earthquake had a sliding surface in the Tokyo Pumice, which is widely distributed in Kanagawa and Tokyo areas (HDS17-04)(abs.)

Authors=CHIGIRA Masahiro, FURUKI Hirokazu, KASAMA Tomohiro, SUZUKI Takehiko

Journal/Book_names=Abstracts, Japan Geoscience Union Meeting (DVD)

volume=2016

pages=HDS17-04

Publish_year=2016

Publish_Country=JPN

Publisher=Japan Geoscience Union

Language_of_Text=JA, EN

ID=201632008