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A Continuous 13.3-Ka Paleoseismic Record Constrains Major Earthquake Recurrence in the Longmen Shan Collision Zone

dc.contributor.authorShi, Wei
dc.contributor.authorJiang, Hanchao
dc.contributor.authorAlsop, G. Ian
dc.contributor.authorWu, Guo
dc.contributor.institutionUniversity of Aberdeen.Geology and Geophysicsen
dc.date.accessioned2022-03-10T14:16:01Z
dc.date.available2022-03-10T14:16:01Z
dc.date.issued2022-03-09
dc.descriptionFUNDING This study is supported by the National Nonprofit Fundamental Research of China Institute of Geology China Earthquake Administration (IGCEA 2126, 1906), the National Natural Science Foundation of China (41572346)en
dc.description.statusPeer revieweden
dc.format.extent11
dc.format.extent2943647
dc.identifier214577343
dc.identifier7442f978-a08d-4bf4-90ca-9f7e54ac7e5e
dc.identifier85127428332
dc.identifier.citationShi, W, Jiang, H, Alsop, G I & Wu, G 2022, 'A Continuous 13.3-Ka Paleoseismic Record Constrains Major Earthquake Recurrence in the Longmen Shan Collision Zone', Frontiers in Earth Science, vol. 10, 838299. https://doi.org/10.3389/feart.2022.838299en
dc.identifier.doi10.3389/feart.2022.838299
dc.identifier.issn2296-6463
dc.identifier.otherBibtex: 10.3389/feart.2022.838299
dc.identifier.otherORCID: /0000-0003-4479-372X/work/161797467
dc.identifier.urihttps://hdl.handle.net/2164/18189
dc.identifier.vol10en
dc.language.isoeng
dc.relation.ispartofFrontiers in Earth Scienceen
dc.subjectsoft sediment deformationen
dc.subjectselsmitesen
dc.subjectmajor earthquakeen
dc.subjectrecurrence timeen
dc.subjectLongmen Shan fault zoneen
dc.subjectEASTERN TIBETAN PLATEAUen
dc.subjectQE Geologyen
dc.subjectSupplementary Informationen
dc.subject.lccQEen
dc.titleA Continuous 13.3-Ka Paleoseismic Record Constrains Major Earthquake Recurrence in the Longmen Shan Collision Zoneen
dc.typeJournal articleen

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