Please use this identifier to cite or link to this item: https://dspace.ctu.edu.vn/jspui/handle/123456789/56301
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dc.contributor.authorLuu, Thi Phuong Lan-
dc.contributor.authorBrooks B., Ellwood-
dc.contributor.authorJonathan H., Tomkin-
dc.contributor.authorGalina P., Nestell-
dc.contributor.authorMerlynd K., Nestell-
dc.contributor.authorKenneth T., Ratcliffe-
dc.contributor.authorHerry, Rowe-
dc.contributor.authorDang, Tran Huyen-
dc.contributor.authorNguyen, Thanh Dung-
dc.contributor.authorNguyen, Chien Thang-
dc.contributor.authorNguyen, Ha Thanh-
dc.contributor.authorDao, Van Quyen-
dc.date.accessioned2021-06-26T12:17:40Z-
dc.date.available2021-06-26T12:17:40Z-
dc.date.issued2018-
dc.identifier.issn0866-7187-
dc.identifier.urihttps://dspace.ctu.edu.vn/jspui/handle/123456789/56301-
dc.description.abstractTwo Permian-Triassic boundary (PTB) successions, Lung Cam in Vietnam, and Lukač in Slovenia, have been sampled for high-resolution magnetic susceptibility, stable isotope and elmental chemistry, and biostratigraphic analyses. These successions are located on the eastern (Lung Cam section) and western margins (Lukač section) of the Paleo-Tethys Ocean during PTB time. Lung Cam, lying along the eastern margin of the Paleo-Tethys Ocean pro-vides an excellent proxy for correlation back to the GSSP and out to other Paleo-Tethyan successions. This proxy is tested herein by correlating the Lung Camsectionin Vietnam to the Lukačsection in Slovenia, which was deposited along the western margin of the Paleo-Tethys Ocean during the PTB interval. It is shown herein that both the Lung Cam and Lukač sections can be correlated andexhibit similar characteristics through the PTB interval. Using time­series analysis of magnetic susceptibility data, high-resolution ages are obtained for both successions, thus allowing relative ages, relative tothe PTB age at ~252 Ma, to be assigned. Evaluation of climate variability along the western and eastern margins of the Paleo-Tethys Ocean through the PTB interval, using δ18Ovalues indicates generally cooler climate in the west, below the PTB, changing to generally warmer climates above the boundary. Aunique Black Car­bon layer (elemental carbon present by agglutinated foraminifers in their test) below the boundary exhibits colder temperatures in the eastern and warmer temperatures in the western Paleo-Tethys Ocean.vi_VN
dc.language.isoenvi_VN
dc.relation.ispartofseriesVietnam Journal of Earth Sciences;No.03, Vol.40 .- P.253–270-
dc.subjectPermain-Triassic boundaryvi_VN
dc.subjectVietnamvi_VN
dc.subjectSloveniavi_VN
dc.subjectTime-series analysisvi_VN
dc.subjectBlack Carbonvi_VN
dc.subjectMagnetostratigraphy susceptibilityvi_VN
dc.subjectHindeodus parvusvi_VN
dc.titleCorrelation and high-resolution timing for Paleo-tethys Permian-Triassic boundary exposures in Vietnam and Slovenia using geochemical, geophysical and biostratigra-phyc data setsvi_VN
dc.typeArticlevi_VN
Appears in Collections:Vietnam journal of Earth sciences

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