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[1] Continental crustal growth and reworking during plate convergence: Implications from Late Mesozoic magmatism in the Southern Qiangtang Terrane, Tibetan Plateau. Geoscience Frontiers. 2026,17 (3):102296
[2] Early Triassic forearc sedimentation in the North Qiangtang terrane, Tibetan Plateau: Implications for northward subduction of the Paleo-Tethys Ocean. SCIENCE CHINA Earth Sciences. 2025,69 (1):313-330
[3] Continental crustal growth and thickness changes caused by the Paleo- to Neo-Tethys Ocean transition: Evidence from the early Jurassic magmatism in the Lhasa terrane. Lithos. 2025
[4] 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
[5] 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
[6] Carboniferous rifting of the Lhasa Terrane (Tibet, China) and the break-up of East Gondwana based on detrital zircon analyses. Palaeogeography, Palaeoclimatology, Palaeoecology. 2024
[7] 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
[8] 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
[9] 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
[10] 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
[11] A greenstone belt in southeast Tibet: An accreted middle–late Permian oceanic plateau. Geoscience Frontiers. 2023
[12] Middle Permian magmatism in the Tangjia-Sumdo region, Tibet: evidence for intra-oceanic subduction.. International Geology Review. 2022
[13] 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
[14] 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
[15] Tectonic Transition from Paleo- to Neo-Tethyan Ocean in Tangjia-Sumdo Area, Southern Tibet: Constraints from Early Jurassic Magmatism.. Gondwana Research. 2022,105 :12-24

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