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主要任职 : 构造教研室主任
其他任职 : 吉林大学青藏高原地质研究中心主任

论文成果当前位置: 中文主页 >> 科学研究 >> 论文成果

[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
[11] 西藏唐加地区石炭纪洋岛型岩石组合及其构造意义. 地球科学. 2022,47 (8):2968-2984
[12] 西藏松多地区超基性岩地球化学特征及对松多古特提斯洋演化的启示. 地质通报. 2022,41 (7):1144-1154
[13] 藏南墨竹工卡叶巴组双峰式火山岩岩石成因、时代及构造环境. 地质通报,41 (8):1369-1381
[14] 藏北羌塘早古生代岩浆作用及其地质意义. 沉积与特提斯地质,41 (2):340-350
[15] 西藏松多古特提斯洋研究进展与存在问题. 沉积与特提斯地质,40 (2):1-13

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