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Chaoming Xie
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Professor
Academic Titles :
Director of Research Center for Tibetan Plateau
Paper Publications
[1]Late Triassic sedimentary environments and detrital zircon provenance analysis in the Amdo area of the Tibetan Plateau: Implications for the evolution of the Meso-Tethys Ocean.Palaeogeography, Palaeoclimatology, Palaeoecology.2024
[2]Subduction of the Proto-Tethys Ocean along the northern margin of Gondwana: Evidence from the Middle Cambrian High-Mg dioritic pluton in the Northern Lhasa Terrane, Tibet.Journal of Asian Earth Sciences.2024
[3]Carboniferous rifting of the Lhasa Terrane (Tibet, China) and the break-up of East Gondwana based on detrital zircon analyses.Palaeogeography, Palaeoclimatology, Palaeoecology.2024
[4]Initial sedimentation after the closure of the Sumdo Paleo-Tethys Ocean: Implications for early Mesozoic tectonics in the East Tethys domain.Lithos.2024(480-481):107668
[5]西藏松多地区蛇纹岩成因及其对松多古特提斯洋俯冲的约束.地球科学.2024,49(3):837-849
[6]Subduction of the Sumdo Paleo-Tethys Oceanic Lithosphere and evolution of the Lhasa Terrane: Inspiration from Middle Triassic Magmatism in Sumdo, Tibet.Lithos.2024,472-473
[7]Provenance of Early Carboniferous clastic sedimentary rocks in the Lhasa Block, Tibet: insights into the paleogeography and tectonic evolution of the northern margin of East Gondwana.Journal of Asian Earth Sciences,256
[8]Opening of the Sumdo Paleo-Tethys Ocean and rifting of the Lhasa terrane from Gondwana: Insights from early Carboniferous magmatism in Southern Tibet.Geological Society of America Bulletin.2023
[9]A greenstone belt in southeast Tibet: An accreted middle–late Permian oceanic plateau.Geoscience Frontiers.2023
[10]Middle Permian magmatism in the Tangjia-Sumdo region, Tibet: evidence for intra-oceanic subduction..International Geology Review.2022
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