Neotectonics of the Eastern Korean Margin Inferred from Back-arc Rifting Structure SCIE SCOPUS KCI
DC Field | Value | Language |
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dc.contributor.author | Kim, Han-Joon | - |
dc.contributor.author | Jou, Hyeong-Tae | - |
dc.contributor.author | Lee, Gwang Hoon | - |
dc.date.accessioned | 2020-04-16T08:40:18Z | - |
dc.date.available | 2020-04-16T08:40:18Z | - |
dc.date.created | 2020-01-28 | - |
dc.date.issued | 2018-09 | - |
dc.identifier.issn | 1738-5261 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/846 | - |
dc.description.abstract | Earthquakes occur frequently in the continental shelf and slope area of the Korean Peninsula in the East Sea (Japan Sea) although they are mostly not large in magnitude. This area constitutes the eastern Korean margin, marking a transitional structure from rifted continental crust to oceanic crust that resulted from lithospheric extension into breakup in a back-arc. We reviewed how the crustal structure of the eastern Korean margin was emplaced to understand its correlation with the present seismicity. Back-arc extension that caused rifting and breakup at the Korean margin took place sequentially from the northern to southern parts in the Late Oligocene through the Early Miocene. The stress regime of the Korean margin switched from extension to compression in the Middle Miocene, resulting from the collision of the Philippine Sea Plate with the Japan Arc. The structural lineations at the Korean margin inherited from backarc rifting and breakup are interpreted to be prone to earthquakes by showing a close spatial correlation with ongoing seismicity. The changing geometry of the estimated locus of breakup at the Korean margin that follows a curvilinear path appears to induce diverse focal mechanisms of the earthquakes under the present compressive stress field. | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | KOREA OCEAN RESEARCH DEVELOPMENT INST | - |
dc.subject | JAPAN SEA | - |
dc.subject | SOUTHWEST JAPAN | - |
dc.subject | CLOCKWISE ROTATION | - |
dc.subject | CONSTRAINTS | - |
dc.subject | EVOLUTION | - |
dc.subject | PLATE | - |
dc.subject | PALEOMAGNETISM | - |
dc.subject | QUATERNARY | - |
dc.subject | MECHANISM | - |
dc.subject | SYSTEM | - |
dc.title | Neotectonics of the Eastern Korean Margin Inferred from Back-arc Rifting Structure | - |
dc.type | Article | - |
dc.citation.endPage | 609 | - |
dc.citation.startPage | 601 | - |
dc.citation.title | OCEAN SCIENCE JOURNAL | - |
dc.citation.volume | 53 | - |
dc.citation.number | 3 | - |
dc.contributor.alternativeName | 김한준 | - |
dc.contributor.alternativeName | 주형태 | - |
dc.identifier.bibliographicCitation | OCEAN SCIENCE JOURNAL, v.53, no.3, pp.601 - 609 | - |
dc.identifier.doi | 10.1007/s12601-018-0036-9 | - |
dc.identifier.scopusid | 2-s2.0-85049065714 | - |
dc.identifier.wosid | 000445435100013 | - |
dc.type.docType | Article | - |
dc.identifier.kciid | ART002385475 | - |
dc.description.journalClass | 1 | - |
dc.subject.keywordPlus | EAST/JAPAN SEA | - |
dc.subject.keywordPlus | SOUTHWEST JAPAN | - |
dc.subject.keywordPlus | CLOCKWISE ROTATION | - |
dc.subject.keywordPlus | CONSTRAINTS | - |
dc.subject.keywordPlus | EVOLUTION | - |
dc.subject.keywordPlus | PLATE | - |
dc.subject.keywordPlus | PALEOMAGNETISM | - |
dc.subject.keywordPlus | QUATERNARY | - |
dc.subject.keywordPlus | MECHANISM | - |
dc.subject.keywordPlus | SYSTEM | - |
dc.subject.keywordAuthor | neotectonics | - |
dc.subject.keywordAuthor | East Sea (Japan Sea) | - |
dc.subject.keywordAuthor | Korean margin | - |
dc.subject.keywordAuthor | back-arc rifting | - |
dc.subject.keywordAuthor | breakup | - |
dc.relation.journalWebOfScienceCategory | Marine & Freshwater Biology | - |
dc.relation.journalWebOfScienceCategory | Oceanography | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.description.journalRegisteredClass | kci | - |
dc.relation.journalResearchArea | Marine & Freshwater Biology | - |
dc.relation.journalResearchArea | Oceanography | - |