Integrated Geophysical Study of the Collision Between the North China Craton and the Yangtze Craton and Its Links With Craton Lithospheric Thinning SCIE SCOPUS

DC Field Value Language
dc.contributor.author Liu, Lihua -
dc.contributor.author Hao, Tianyao -
dc.contributor.author Lü, Chuanchuan -
dc.contributor.author Wu, Zhiqiang -
dc.contributor.author Kim, Kwanghee -
dc.contributor.author Kim, Han Joon -
dc.contributor.author Xu, Ya -
dc.date.accessioned 2022-02-28T00:50:06Z -
dc.date.available 2022-02-28T00:50:06Z -
dc.date.created 2022-02-28 -
dc.date.issued 2022-01 -
dc.identifier.issn 2296-6463 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/42366 -
dc.description.abstract Unlike stable cratons elsewhere in the world, the lithosphere is strongly thinned in the east of both the North China Craton (NCC) and the Yangtze Craton (YZC) compared with the west. We deployed four active-source onshore-offshore wide-angle seismic survey lines in the eastern NCC and YZC from 2010 to 2016 with the aim of revealing the mechanism of lithospheric thinning and the process of the collision between the NCC and YZC. We obtained high-resolution crustal P-wave velocity models for the eastern NCC and YZC based on seismic forward modeling, travel-time tomography, and finite-difference wave-field modeling. Based on our integrated geophysical study and previous work, we propose a five-stage model for the collision between the YZC and NCC, with different dominant geodynamic mechanisms in each stage. Our collision model shows that lithospheric thinning in the eastern NCC and YZC is a consequence of the NCC-YZC collision and subduction of the Pacific plate. Copyright © 2022 Liu, Hao, Lü, Wu, Kim, Kim and Xu. -
dc.description.uri 1 -
dc.language English -
dc.publisher Frontiers Media S.A. -
dc.title Integrated Geophysical Study of the Collision Between the North China Craton and the Yangtze Craton and Its Links With Craton Lithospheric Thinning -
dc.type Article -
dc.citation.title Frontiers in Earth Science -
dc.citation.volume 9 -
dc.contributor.alternativeName 김한준 -
dc.identifier.bibliographicCitation Frontiers in Earth Science, v.9 -
dc.identifier.doi 10.3389/feart.2021.796783 -
dc.identifier.scopusid 2-s2.0-85124756295 -
dc.identifier.wosid 000757194300001 -
dc.type.docType Article -
dc.description.journalClass 1 -
dc.description.isOpenAccess N -
dc.subject.keywordPlus PRESSURE METAMORPHIC ROCKS -
dc.subject.keywordPlus CRUSTAL STRUCTURE BENEATH -
dc.subject.keywordPlus SOURCE SEISMIC EXPERIMENT -
dc.subject.keywordPlus METALLOGENIC BELT -
dc.subject.keywordPlus CONTINENTAL SUBDUCTION -
dc.subject.keywordPlus DABIE MOUNTAINS -
dc.subject.keywordPlus VELOCITY MODEL -
dc.subject.keywordPlus YELLOW SEA -
dc.subject.keywordPlus EXHUMATION -
dc.subject.keywordPlus MIDDLE -
dc.subject.keywordAuthor crustal structure -
dc.subject.keywordAuthor lithospheric thinning -
dc.subject.keywordAuthor North China Craton -
dc.subject.keywordAuthor sulu orogenic belt -
dc.subject.keywordAuthor wide-angle seismic survey -
dc.subject.keywordAuthor Yangtze Craton -
dc.relation.journalWebOfScienceCategory Geosciences, Multidisciplinary -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.relation.journalResearchArea Geology -
Appears in Collections:
Ocean Climate Solutions Research Division > Ocean Climate Response & Ecosystem Research Department > 1. Journal Articles
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