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DC Field | Value | Language |
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dc.contributor.author | Luu, Thi Phuong Lan | - |
dc.contributor.author | Brooks B., Ellwood | - |
dc.contributor.author | Jonathan H., Tomkin | - |
dc.contributor.author | Galina P., Nestell | - |
dc.contributor.author | Merlynd K., Nestell | - |
dc.contributor.author | Kenneth T., Ratcliffe | - |
dc.contributor.author | Herry, Rowe | - |
dc.contributor.author | Dang, Tran Huyen | - |
dc.contributor.author | Nguyen, Thanh Dung | - |
dc.contributor.author | Nguyen, Chien Thang | - |
dc.contributor.author | Nguyen, Ha Thanh | - |
dc.contributor.author | Dao, Van Quyen | - |
dc.date.accessioned | 2021-06-26T12:17:40Z | - |
dc.date.available | 2021-06-26T12:17:40Z | - |
dc.date.issued | 2018 | - |
dc.identifier.issn | 0866-7187 | - |
dc.identifier.uri | https://dspace.ctu.edu.vn/jspui/handle/123456789/56301 | - |
dc.description.abstract | Two 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.iso | en | vi_VN |
dc.relation.ispartofseries | Vietnam Journal of Earth Sciences;No.03, Vol.40 .- P.253–270 | - |
dc.subject | Permain-Triassic boundary | vi_VN |
dc.subject | Vietnam | vi_VN |
dc.subject | Slovenia | vi_VN |
dc.subject | Time-series analysis | vi_VN |
dc.subject | Black Carbon | vi_VN |
dc.subject | Magnetostratigraphy susceptibility | vi_VN |
dc.subject | Hindeodus parvus | vi_VN |
dc.title | Correlation and high-resolution timing for Paleo-tethys Permian-Triassic boundary exposures in Vietnam and Slovenia using geochemical, geophysical and biostratigra-phyc data sets | vi_VN |
dc.type | Article | vi_VN |
Appears in Collections: | Vietnam journal of Earth sciences |
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