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Tectonic Features along the South Scotia Ridge, Antarctica

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dc.contributor.authorPark, Minkyu-
dc.contributor.authorHong, Jong Kuk-
dc.contributor.authorNam, SangHeon-
dc.contributor.authorLee, Ju-Han-
dc.contributor.authorJin, Young Keun-
dc.coverage.spatialAntarctic sea-
dc.date.accessioned2018-03-20T13:20:05Z-
dc.date.available2018-03-20T13:20:05Z-
dc.date.issued2005-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/5948-
dc.description.abstractMultichannel seismic survey has conducted along the South Scotia Ridge which is located in the northernpart of Weddell sea, Antarctic sea. The South Scotia Ridge is part of continental crust extended fromAntarctic Peninsula. It borders on Oceanic plates, the Scotia sea plate and Powell basin. Transtensionaltectonics along the sinistral transform fault plate boundary led to the creation of the present tectonicgeomorphology of the South Scotia Ridge. The fan-shaped deposits with angular unconformities inthe central depression is interpreted as a divergent tectonic movement along the ridge.-
dc.languageKorean-
dc.subjectEnvironmental Sciences & Ecology-
dc.titleTectonic Features along the South Scotia Ridge, Antarctica-
dc.title.alternative남극해 남스코시아 해령 주변의 지체구조-
dc.typeArticle-
dc.identifier.bibliographicCitationPark, Minkyu, et al. 2005. "Tectonic Features along the South Scotia Ridge, Antarctica". <em>Korean Geophysical Society</em>, 8(4): 215-219.-
dc.citation.titleKorean Geophysical Society-
dc.citation.volume8-
dc.citation.number4-
dc.citation.startPage215-
dc.citation.endPage219-
dc.description.articleClassificationKCI등재후보-
dc.description.jcrRateJCR 2003:0-
dc.subject.keywordSouth Scotia Ridge-
dc.subject.keywordAntarctic sea-
dc.subject.keywordSeismic survey-
dc.subject.keywordtranstensional tectonics-
dc.subject.keywordcentral depression-
dc.identifier.localId2005-0129-
Appears in Collections  
2004-2010, Antarctic Marine Geological Survey (04-10) / Hong, Jong Kuk; Nam, SangHeon
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