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
About this item
Full title
Author / Creator
Publisher
Berlin/Heidelberg: Springer Berlin Heidelberg
Journal title
Language
English
Formats
Publication information
Publisher
Berlin/Heidelberg: Springer Berlin Heidelberg
Subjects
More information
Scope and Contents
Contents
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 region, posing a major seismic hazard potential to the coast...
Alternative Titles
Full title
Shallow structure and late quaternary slip rate of the Osaka Bay fault, western Japan
Authors, Artists and Contributors
Identifiers
Primary Identifiers
Record Identifier
TN_cdi_doaj_primary_oai_doaj_org_article_f8f5f156c3104ab99c02b1381aa6a8f5
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_f8f5f156c3104ab99c02b1381aa6a8f5
Other Identifiers
ISSN
2197-4284
E-ISSN
2197-4284
DOI
10.1186/s40645-024-00607-0
