Seismic character of the BSR in the Ulleung Basin plain, East Sea (Japan Sea) SCIE SCOPUS KCI

DC Field Value Language
dc.contributor.author Kim, Han-Joon -
dc.contributor.author Lee, Gwan Hoon -
dc.contributor.author Jou, Hyeong-Tae -
dc.contributor.author Lee, Sang Hoon -
dc.contributor.author Yoo, Dong-Geun -
dc.contributor.author Koo, Nam-Hyung -
dc.contributor.author Jeong, Gap-Sik -
dc.contributor.author Suk, Ong-Chool -
dc.date.accessioned 2020-04-20T08:55:07Z -
dc.date.available 2020-04-20T08:55:07Z -
dc.date.created 2020-01-28 -
dc.date.issued 2010-03 -
dc.identifier.issn 1226-4806 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/4132 -
dc.description.abstract A bottom simulating reflector (BSR) was identified in in seismic reflection profiles collected in the filleting Basin plain, East Sea (Japan Sea). The BSR, occurring in densely stratified sediments, is observed very close to the boundary between two sequences interpreted as low-energy turbidites/hemipelagic sediments and mass-transport deposits. The essential characteristics of the BSR include its cross-cutting relationship to strata at a small angle, strong amplitude, and reverse polarity with respect to the seafloor reflection. Stochastic inversion of seismic data indicates that the BSR reflect ion coefficients reach in the range from 0.23 to 0.26 and are 1.5 similar to 1.7 times that of the sea floor reflection. A decrease in interval velocities, disrupted seismic signals, and noticeable drop of the frequency content are recognized below the BSR. These features strongly suggest that the BSR represents the base of gas hydrate stability zone (BHSZ) in the Ulleung Basin plain and a free gas zone is present below the BSR with high amplitude. Inversion also discriminates the lower amplitude BSR that is not easily identified from interfering reflection signals, suggesting that gas hydrates exist more extensively in the filleting Basin than recognized in seismic profiles. -
dc.description.uri 1 -
dc.language English -
dc.publisher SPRINGER HEIDELBERG -
dc.subject GAS HYDRATE -
dc.subject SEDIMENTS -
dc.title Seismic character of the BSR in the Ulleung Basin plain, East Sea (Japan Sea) -
dc.type Article -
dc.citation.endPage 55 -
dc.citation.startPage 49 -
dc.citation.title GEOSCIENCES JOURNAL -
dc.citation.volume 14 -
dc.citation.number 1 -
dc.identifier.bibliographicCitation GEOSCIENCES JOURNAL, v.14, no.1, pp.49 - 55 -
dc.identifier.doi 10.1007/s12303-010-0006-4 -
dc.identifier.scopusid 2-s2.0-77952028809 -
dc.identifier.wosid 000276307500006 -
dc.type.docType Article -
dc.identifier.kciid ART001429928 -
dc.description.journalClass 1 -
dc.subject.keywordPlus GAS HYDRATE -
dc.subject.keywordPlus SEDIMENTS -
dc.subject.keywordAuthor Ulleung Basin -
dc.subject.keywordAuthor BSR -
dc.subject.keywordAuthor gas hydrate -
dc.subject.keywordAuthor seismic profile -
dc.subject.keywordAuthor stochastic inversion -
dc.relation.journalWebOfScienceCategory Geosciences, Multidisciplinary -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.description.journalRegisteredClass kci -
dc.relation.journalResearchArea Geology -
Appears in Collections:
Marine Environmental & Climate Research Division > Marine Active Fault Research Unit > 1. Journal Articles
Marine Domain Management Research Division > Korean Seas Geosystem Research Unit > 1. Journal Articles
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