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Article: Reconstruction of the Holocene seismic history of a seabed fault using relative sea-level curves reconstructed by ostracode assemblages: Case study on the Median Tectonic Line in Iyo-nada Bay, western Japan

TitleReconstruction of the Holocene seismic history of a seabed fault using relative sea-level curves reconstructed by ostracode assemblages: Case study on the Median Tectonic Line in Iyo-nada Bay, western Japan
Authors
KeywordsHolocene
Japan
Ostracoda
Relative sea-level change
Seabed fault
Seismic history
Issue Date2005
PublisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/palaeo
Citation
Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, v. 222 n. 3-4, p. 285-312 How to Cite?
AbstractRelative sea-level curves of cores K1, K2, S1, and S2 collected from Iyo-nada Bay, western Japan, were reconstructed using ostracode assemblages. These curves clearly show a Holocene history of seismic subsidence. Comparing the curves with sea-level histories from a tectonically stable area of Japan demonstrates that Iyo-nada Bay has undergone subsidence through the Holocene. This subsidence was probably caused by movements of the Median Tectonic Line (MTL) fault system in Iyo-nada Bay. Comparison of relative sea-level curves of the lower and upper plates elucidated a detailed seismic history of the Kaminada-oki-kita and Shimonada-oki-minami Faults. The Kaminada-oki-kita Fault moved vertically about 7 m at ca. 5500-0 cal yr BP, in addition this fault may have moved vertically about 5 m, and 9 m at ca. 7500-6000 cal yr BP and ca. 10,000-9000 cal yr BP, respectively. The Shimonada-oki-minami Fault has moved vertically about 15 m over the last 6500 years. This fault also might have had a large movement around 10,000 cal yr BP. This study provided a robust method for reconstruction of the Holocene seismic history using ostracode assemblages found in seabed drilling cores. © 2005 Elsevier B.V. All rights reserved.
Persistent Identifierhttp://hdl.handle.net/10722/132801
ISSN
2015 Impact Factor: 2.525
2015 SCImago Journal Rankings: 1.501
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorYasuhara, Men_HK
dc.contributor.authorYoshikawa, Sen_HK
dc.contributor.authorNanayama, Fen_HK
dc.date.accessioned2011-03-28T09:29:10Z-
dc.date.available2011-03-28T09:29:10Z-
dc.date.issued2005en_HK
dc.identifier.citationPalaeogeography, Palaeoclimatology, Palaeoecology, 2005, v. 222 n. 3-4, p. 285-312en_HK
dc.identifier.issn0031-0182en_HK
dc.identifier.urihttp://hdl.handle.net/10722/132801-
dc.description.abstractRelative sea-level curves of cores K1, K2, S1, and S2 collected from Iyo-nada Bay, western Japan, were reconstructed using ostracode assemblages. These curves clearly show a Holocene history of seismic subsidence. Comparing the curves with sea-level histories from a tectonically stable area of Japan demonstrates that Iyo-nada Bay has undergone subsidence through the Holocene. This subsidence was probably caused by movements of the Median Tectonic Line (MTL) fault system in Iyo-nada Bay. Comparison of relative sea-level curves of the lower and upper plates elucidated a detailed seismic history of the Kaminada-oki-kita and Shimonada-oki-minami Faults. The Kaminada-oki-kita Fault moved vertically about 7 m at ca. 5500-0 cal yr BP, in addition this fault may have moved vertically about 5 m, and 9 m at ca. 7500-6000 cal yr BP and ca. 10,000-9000 cal yr BP, respectively. The Shimonada-oki-minami Fault has moved vertically about 15 m over the last 6500 years. This fault also might have had a large movement around 10,000 cal yr BP. This study provided a robust method for reconstruction of the Holocene seismic history using ostracode assemblages found in seabed drilling cores. © 2005 Elsevier B.V. All rights reserved.en_HK
dc.languageengen_US
dc.publisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/palaeoen_HK
dc.relation.ispartofPalaeogeography, Palaeoclimatology, Palaeoecologyen_HK
dc.subjectHoloceneen_HK
dc.subjectJapanen_HK
dc.subjectOstracodaen_HK
dc.subjectRelative sea-level changeen_HK
dc.subjectSeabed faulten_HK
dc.subjectSeismic historyen_HK
dc.titleReconstruction of the Holocene seismic history of a seabed fault using relative sea-level curves reconstructed by ostracode assemblages: Case study on the Median Tectonic Line in Iyo-nada Bay, western Japanen_HK
dc.typeArticleen_HK
dc.identifier.emailYasuhara, M: yasuhara@hku.hken_HK
dc.identifier.authorityYasuhara, M=rp01474en_HK
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.doi10.1016/j.palaeo.2005.03.019en_HK
dc.identifier.scopuseid_2-s2.0-20544465187en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-20544465187&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume222en_HK
dc.identifier.issue3-4en_HK
dc.identifier.spage285en_HK
dc.identifier.epage312en_HK
dc.identifier.isiWOS:000230440300005-
dc.publisher.placeNetherlandsen_HK
dc.identifier.scopusauthoridYasuhara, M=7102069020en_HK
dc.identifier.scopusauthoridYoshikawa, S=7202952155en_HK
dc.identifier.scopusauthoridNanayama, F=6602798032en_HK

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