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

dc.contributor.authorHamahashi, Mari
dc.contributor.authorOtsuka, Hironori
dc.contributor.authorSuzuki, Yoshiaki
dc.contributor.authorArimoto, Jun
dc.contributor.authorMatsuno, Tetsuo
dc.contributor.authorSeama, Nobukazu
dc.contributor.authorYamamoto, Yuzuru
dc.contributor.authorSugioka, Hiroko
dc.contributor.authorBowden, Stephen A.
dc.contributor.authorShimizu, Satoshi
dc.contributor.authorIwamaru, Hikaru
dc.contributor.authorSano, Mamoru
dc.contributor.authorSuzuki, Keita
dc.contributor.authorKaneko, Katsuya
dc.contributor.authorNakahigashi, Kazuo
dc.contributor.authorTatsumi, Yoshiyuki
dc.contributor.institutionUniversity of Aberdeen.Geology and Geophysicsen
dc.date.accessioned2024-07-19T10:55:01Z
dc.date.available2024-07-19T10:55:01Z
dc.date.issued2024-02-14
dc.descriptionWe are grateful to Editor Ken Ikehara for handling our manuscript, and to Karl Mueller and an anonymous reviewer for their constructive and insightful reviews that have helped improve this contribution. We express our gratitude to Yoshiji Yano, Masaki Fuchi, and crew members of the T/S Fukaemaru for the operation of the ship during our surveys. We are grateful to Morihito Ishu for the operation of the R/V Onokoro, and Masata Suzuki and Satomi Takagi for their assistance on the ship. We are thankful to Shinya Uwai and staff members from the Research Center for Inland Seas, Kobe University (KURCIS) for their hospitality during our stay at the Marine Site (Joint Usage/Education Center of MEXT). We are grateful to Takahiko Inoue, Ayanori Misawa, Tomoyuki Sato, Fumitoshi Murakami, Kohsaku Arai, and Rei Nakashima for useful discussions. We are thankful to Takuya Nishimura for the valuable discussions and insights on geodetic strain rates around the Osaka Bay. We express our gratitude to Tomoichi Enomoto, Shin Terado, Mitsutec Corp., Hiruzen Institute for Geology and Chronology Co., Ltd., Masayoshi Kondo, Nakagawa Textile Co., Ltd., and Seisgadget Ltd., for their contribution in the academic crowdfunding to investigate the active faults in the Osaka Bay (Academist Project #111). We thank all the students and staffs that have participated in the seismic surveys during the marine geophysics field class held during the period of 2017–2021 onboard the T/S Fukaemaru at Kobe University.en
dc.description.statusPeer revieweden
dc.format.extent50
dc.format.extent32606790
dc.identifier289641685
dc.identifierc93b4b96-88f8-4ce3-95cc-7b7d4a5bb0cb
dc.identifier85185337437
dc.identifier.citationHamahashi, M, Otsuka, H, Suzuki, Y, Arimoto, J, Matsuno, T, Seama, N, Yamamoto, Y, Sugioka, H, Bowden, S A, Shimizu, S, Iwamaru, H, Sano, M, Suzuki, K, Kaneko, K, Nakahigashi, K & Tatsumi, Y 2024, 'Shallow structure and late quaternary slip rate of the Osaka Bay fault, western Japan', Progress in Earth and Planetary Science, vol. 11, 8. https://doi.org/10.1186/s40645-024-00607-0en
dc.identifier.doi10.1186/s40645-024-00607-0
dc.identifier.issn2197-4284
dc.identifier.urihttps://hdl.handle.net/2164/23863
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=85185337437&partnerID=8YFLogxKen
dc.identifier.vol11en
dc.language.isoeng
dc.relation.ispartofProgress in Earth and Planetary Scienceen
dc.subjectBoreholesen
dc.subjectGrowth strataen
dc.subjectKinki triangleen
dc.subjectLate quaternary sedimentsen
dc.subjectMulti-beam bathymetryen
dc.subjectNiigata–Kobe tectonic zoneen
dc.subjectOsaka Bay faulten
dc.subjectSedimentary basinsen
dc.subjectSeismic reflection surveyen
dc.subjectSlip rateen
dc.subjectQE Geologyen
dc.subjectGeneral Earth and Planetary Sciencesen
dc.subject.lccQEen
dc.titleShallow structure and late quaternary slip rate of the Osaka Bay fault, western Japanen
dc.typeJournal articleen

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