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Rate of late Quaternary ice-cap thinning on King George Island, South Shetland Islands, West Antarctica definded by cosmogenic 36Cl surface exposure dating

Cited 24 time in wos
Cited 24 time in scopus

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DC Field Value Language
dc.contributor.authorSeong, Y.B.-
dc.contributor.authorL.A. Owen-
dc.contributor.authorLee, Yong Il-
dc.contributor.authorM.W. Caffee-
dc.contributor.authorKim, Yeadong-
dc.contributor.authorYoon, Ho Il-
dc.contributor.authorLim, Hyoun Soo-
dc.coverage.spatialAntarctica-
dc.coverage.spatialBarton Peninsula-
dc.coverage.spatialKing George Island-
dc.coverage.spatialSouth Shetland Islands-
dc.coverage.spatialWeaver Peninsula-
dc.date.accessioned2018-03-20T13:38:01Z-
dc.date.available2018-03-20T13:38:01Z-
dc.date.issued2009-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/6020-
dc.description.abstractGlacial landforms on the Barton and Weaver peninsulas of King George Island in the South Shetland Islands, West Antarctica were mapped and dated using terrestrial cosmogenic 36Cl methods to provide the first quantitative terrestrial record for late Quaternary deglaciation in the South Shetland Islands. 36Cl ages on glacially eroded and striated bedrock surfaces range from 15.5+2.5 kyr to 1.0+0.7 kyr. The 36Cl ages are younger with decreasing altitude, indicating progressive downwasting of the southwestern part of the Collins Ice Cap at a rate of -12mm/yr since 15.5+2.5 kyr ago, supporting the previously published marine records for the timing and estimate of the rate of deglaciation in this region.-
dc.languageEnglish-
dc.publisherTAYLOR & FRANCIS-
dc.subjectPhysical Geography-
dc.subjectGeology-
dc.titleRate of late Quaternary ice-cap thinning on King George Island, South Shetland Islands, West Antarctica definded by cosmogenic 36Cl surface exposure dating-
dc.title.alternative36Cl 노출연대측정을 이용한 서남극 남셰틀랜드군도 킹죠지섬의 제4기 후기 빙모 감소속도 연구-
dc.typeArticle-
dc.identifier.bibliographicCitationSeong, Y.B., et al. 2009. "Rate of late Quaternary ice-cap thinning on King George Island, South Shetland Islands, West Antarctica definded by cosmogenic 36Cl surface exposure dating". <em>Boreas</em>, 38: 207-213.-
dc.citation.titleBoreas-
dc.citation.volume38-
dc.identifier.doi10.1111/j.1502-3885.2008.00069.x-
dc.citation.startPage207-
dc.citation.endPage213-
dc.description.articleClassificationSCI-
dc.description.jcrRateJCR 2007:23.35766423357664-
dc.subject.keywordAntarctica-
dc.subject.keywordKing George Island-
dc.subject.keywordLGM-
dc.subject.keywordcosmogenic 36Cl dating-
dc.subject.keyworddeglaciation-
dc.identifier.localId2009-0052-
dc.identifier.scopusid2-s2.0-73649088651-
dc.identifier.wosid000264563700002-
Appears in Collections  
2007-2010, Studies on the soil geochemistry and patterned ground in the polar regions: implications for paleoclimatic and paleoenvironmental changes during the late Quaternary (07-10) / Yoon, Ho Il (PN08020, PN09020, PN07040)
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