Flexural isostasy and loading sequence of the Dokdo seamounts on the Ulleung Basin in the East Sea (Sea of Japan) SCIE SCOPUS

DC Field Value Language
dc.contributor.author Kim, Chang Hwan -
dc.contributor.author Park, Chan Hong -
dc.contributor.author Jeong, Eui Young -
dc.contributor.author Ko, Young Tak -
dc.contributor.author Hwang, Jong Sun -
dc.contributor.author Shim, Taek Mo -
dc.date.accessioned 2020-04-20T09:40:21Z -
dc.date.available 2020-04-20T09:40:21Z -
dc.date.created 2020-01-28 -
dc.date.issued 2009-08-03 -
dc.identifier.issn 1367-9120 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/4265 -
dc.description.abstract The isostatic compensation and loading sequence of the Dokdo seamounts on the Ulleung Basin in the East Sea are studied by a flexure model using gravity and bathymetric data. The Dokdo seamounts comprise Dokdo (Dok Island), lying as a cluster of emerged small islets surmounting a large submerged volcanic edifice, and two voluminous tablemounts, Simheungtaek and Isabu. In spite of their similarity in topographic expression, a large difference of about 50 mGal between the observed gravity anomaly peaks over Dokdo and the Isabu Tablemount implies different amounts of compensation. A comparison between the observed and calculated gravity anomalies of the seamounts shows that the flexural compensation investigated in this study predicts well the observed data. The flexure model suggests that the Dokdo seamounts might be composed of high-density volcanic rocks. Modeling results show that the flexural rigidity or effective elastic thickness of the lithosphere under Dokdo is stronger or thicker than that under the Isabu Tablemount. it implies that the age of lithosphere at the time of loading for Isabu was younger than that for Dokdo. The effective elastic thicknesses associated with the Dokdo seamounts approximately follow 200-400 degrees C isotherms in the cooling plate model. The results of this study and the former age dating of Dokdo suggest that the Isabu Tablemount was formed first, followed by Dokdo after the opening of the East Sea ceased. (C) 2009 Elsevier Ltd. All rights reserved. -
dc.description.uri 1 -
dc.language English -
dc.publisher PERGAMON-ELSEVIER SCIENCE LTD -
dc.subject BACK-ARC BASIN -
dc.subject OPENING MODE -
dc.subject ELASTIC THICKNESS -
dc.subject CRUSTAL STRUCTURE -
dc.subject ISLANDS -
dc.subject PALEOMAGNETISM -
dc.subject LITHOSPHERE -
dc.subject VOLCANISM -
dc.subject MARGIN -
dc.subject DEFORMATION -
dc.title Flexural isostasy and loading sequence of the Dokdo seamounts on the Ulleung Basin in the East Sea (Sea of Japan) -
dc.type Article -
dc.citation.endPage 468 -
dc.citation.startPage 459 -
dc.citation.title JOURNAL OF ASIAN EARTH SCIENCES -
dc.citation.volume 35 -
dc.citation.number 5 -
dc.identifier.bibliographicCitation JOURNAL OF ASIAN EARTH SCIENCES, v.35, no.5, pp.459 - 468 -
dc.identifier.doi 10.1016/j.jseaes.2009.02.009 -
dc.identifier.scopusid 2-s2.0-67349279406 -
dc.identifier.wosid 000267237700007 -
dc.type.docType Article -
dc.description.journalClass 1 -
dc.subject.keywordPlus BACK-ARC BASIN -
dc.subject.keywordPlus OPENING MODE -
dc.subject.keywordPlus ELASTIC THICKNESS -
dc.subject.keywordPlus CRUSTAL STRUCTURE -
dc.subject.keywordPlus ISLANDS -
dc.subject.keywordPlus PALEOMAGNETISM -
dc.subject.keywordPlus LITHOSPHERE -
dc.subject.keywordPlus VOLCANISM -
dc.subject.keywordPlus MARGIN -
dc.subject.keywordPlus DEFORMATION -
dc.subject.keywordAuthor Isostatic compensation -
dc.subject.keywordAuthor Dokdo seamounts -
dc.subject.keywordAuthor Flexure model -
dc.subject.keywordAuthor Cooling plate model -
dc.relation.journalWebOfScienceCategory Geosciences, Multidisciplinary -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.relation.journalResearchArea Geology -
Appears in Collections:
Marine Resources Research Division > Deep-sea Mineral Resources Research Center > 1. Journal Articles
East Sea Research Institute > East Sea Environment Research Center > 1. Journal Articles
East Sea Research Institute > Dokdo Research Center > 1. Journal Articles
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