Shallow structure and late quaternary slip rate of the Osaka Bay fault, western Japan

Shallow structure and late quaternary slip rate of the Osaka Bay fault, western Japan

Abstract The Osaka Bay is situated at a seismically active region north of the Median Tectonic Line and east of Awaji Island in western Japan, known as part of the Kinki Triangle and the Niigata–Kobe Tectonic Zone. Dense distribution of active faults and high geodetic strain rates characterize the r...

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Bibliographic Details
Main Authors: Mari Hamahashi, Hironori Otsuka, Yoshiaki Suzuki, Jun Arimoto, Tetsuo Matsuno, Nobukazu Seama, Yuzuru Yamamoto, Hiroko Sugioka, Stephen A. Bowden, Satoshi Shimizu, Hikaru Iwamaru, Mamoru Sano, Keita Suzuki, Katsuya Kaneko, Kazuo Nakahigashi, Yoshiyuki Tatsumi
Format: Article
Language:English
Published: SpringerOpen 2024-02-01
Series:Progress in Earth and Planetary Science
Subjects:
Seismic reflection survey
Multi-beam bathymetry
Osaka Bay fault
Slip rate
Late quaternary sediments
Growth strata
Online Access:https://doi.org/10.1186/s40645-024-00607-0

Internet

https://doi.org/10.1186/s40645-024-00607-0

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