Was the Ulleung Basin (Tsushima basin) formed above the hotter than normal mantle?

DC Field Value Language
dc.contributor.author 김한준 -
dc.date.accessioned 2020-07-17T04:51:18Z -
dc.date.available 2020-07-17T04:51:18Z -
dc.date.created 2020-02-11 -
dc.date.issued 2007-03-01 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/30670 -
dc.description.abstract The SE Korean margin in the East Sea consists of the continental shelf and slope passing into the Ulleung Basin. In this study, I summorized the results of deep seismic sounding experiments emplying ocean bottom seismometers to investigate the crustal structure and nature from the Korean margin to the Ulleung Basin. I further discuss the architecture of continental rifting at the Korean margin based on multichannel seismic profiles -
dc.description.uri 1 -
dc.language English -
dc.publisher Niigata Univ. -
dc.relation.isPartOf 2006 Japan-Korea Joint Symp. on Ocean Drilling -
dc.title Was the Ulleung Basin (Tsushima basin) formed above the hotter than normal mantle? -
dc.type Conference -
dc.citation.conferencePlace JA -
dc.citation.endPage 54 -
dc.citation.startPage 51 -
dc.citation.title 2006 Japan-Korea Joint Symp. on Ocean Drilling -
dc.contributor.alternativeName 김한준 -
dc.identifier.bibliographicCitation 2006 Japan-Korea Joint Symp. on Ocean Drilling, pp.51 - 54 -
dc.description.journalClass 1 -
Appears in Collections:
Ocean Climate Solutions Research Division > Ocean Climate Response & Ecosystem Research Department > 2. Conference Papers
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