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Crust and upper mantle structure beneath the Yellow Sea region using receiver function analysis

Cited 1 time in wos
Cited 1 time in scopus

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DC Field Value Language
dc.contributor.authorYu, Chanho-
dc.contributor.authorPaul-
dc.contributor.authorXu-
dc.contributor.authorKim, Kwang-Hee-
dc.contributor.authorPark, Yongcheol-
dc.contributor.authorKang, Suyoung-
dc.contributor.authorSuk, Bongchool-
dc.contributor.authorSuh, Mancheol-
dc.coverage.spatialPacific Ocean-
dc.coverage.spatialYellow Sea-
dc.date.accessioned2018-03-20T13:40:21Z-
dc.date.available2018-03-20T13:40:21Z-
dc.date.issued2010-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/6081-
dc.description.abstractTeleseismic events are used to obtain shear-wave velocity models beneath the stations of the Yellow Sea Broadband Seismic Network (YSBSN). Some stations are located on top of either a thick sedimentary basin or highly porous volcanic rocks and receiver functions at these stations exhibit prominent high-amplitude and long-period reverberations which obscure the subtle phases associated with deeper structures. Due to the shallow subsurface effects in receiver functions, shear-wave velocity models beneath only 8 broadband seismic stations are successfully inverted. Depth to the crust?antle transition (the Moho) varies from 30 to 38 km beneath YSBSN stations. The thickest crust is observed beneath the station JNN in China, which is attributed to the ancient collision boundary between the North China block and the South China block. Although general increase of the crustal thickness from north to south in Korea is observed with high confidence, it is not possible to delineate the location of potential collision boundary in the southern Korea peninsula, which would require wider coverage by broadband seismic instruments to resolve.-
dc.language중국어-
dc.publisherThe Chinese Geophysical Society-
dc.subjectGeochemistry & Geophysics-
dc.titleCrust and upper mantle structure beneath the Yellow Sea region using receiver function analysis-
dc.title.alternative수신함수 분석을 이용한 황해지역의 지각 및 상부 맨틀 속도-
dc.typeArticle-
dc.identifier.bibliographicCitationYu, Chanho, et al. 2010. "Crust and upper mantle structure beneath the Yellow Sea region using receiver function analysis". <em>CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION</em>, 53(6): 1336-1343.-
dc.citation.titleCHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION-
dc.citation.volume53-
dc.citation.number6-
dc.identifier.doi10.3969/j.issn.0001-5733.2010.06.012-
dc.citation.startPage1336-
dc.citation.endPage1343-
dc.description.articleClassificationSCIE-
dc.description.jcrRateJCR 2008:79.6875-
dc.subject.keywordP-to-S converted wave-
dc.subject.keywordYellow Sea-
dc.subject.keywordreceiver function-
dc.subject.keywordteleseismic event-
dc.subject.keywordvelocity model-
dc.identifier.localId2010-0075-
dc.identifier.scopusid2-s2.0-78650100166-
dc.identifier.wosid000279445500012-
Appears in Collections  
2006-2010, Constructing Polar Monitoring-Network System: Studies on Characteristics of Submarine Active Tectonic Processes and Marine Environmental Changes (06-10) / Park, Minkyu (PP10020, PP09020, PP07020, PP06020, PP08020)
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