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dc.contributor.authorHuangh, Yuanhuien
dc.contributor.authorLan, Dongzhaoen
dc.coverage.spatialthe Northeastern South China Seaen
dc.date.accessioned2015-01-21T04:31:57Z
dc.date.available2015-01-21T04:31:57Z
dc.date.issued2007en
dc.identifier.citationMarine Science Bulletin, 9 (1), 46-54en
dc.identifier.issn1000-9620*
dc.identifier.urihttp://hdl.handle.net/1834/5836
dc.description.abstractCore D(21°23′02″N,116°47′13″E, water depth 405 m)was sampled from the upper slope from the northeastern South China Sea (SCS) and applied to analyze the sedimentary environmental change in this sea area since the last glacial stage. The results of grain size analysis, diatom analysis and detrital mineral analysis were well matched. We divided the core D into two layers. The surface sand layer (0 - 2 cm) consisted of residual sediments, which might be originally the sediment in the late Pleistocene and later suffered from being transformed in the post glacial transgression. The lower layer (2 - 130 cm) was quite different from the surface one, which might mainly result from a neritic sedimentary environment in the last glacial stage. Two sedimentary cycles could be detected in the core D: regression during Marine isotope stage (MIS) 4 to transgression during MIS 3 and regression during MIS 2 to transgression during the post glacial.en
dc.language.isoenen
dc.rights.urihttp://creativecommons.org/licenses/by-nc/3.0/en
dc.titleDevelopment of Sedimentary Environment in the Northeastern South China Sea Since the Last Glacial Stage.en
dc.typeJournal Contribution*
dc.bibliographicCitation.endpage54en
dc.bibliographicCitation.issue1en
dc.bibliographicCitation.stpage46en
dc.bibliographicCitation.titleMarine Science Bulletinen
dc.bibliographicCitation.volume9en
dc.description.statusPublisheden
dc.description.otherthe last glacial stageen
dc.subject.asfaGrain sizeen
dc.subject.asfaDiatomsen
dc.subject.asfaSedimentary environmentsen
dc.type.refereedNon-Refereeden
dc.type.specifiedArticleen
refterms.dateFOA2021-01-30T18:48:19Z


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