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[1] 东北亚大地幔楔水-碳循环及其效应: 新生代玄武岩地球化学制. 岩石学报. 2025,41 (12):4107-4125
[2] Deep carbon cycling due to m´elange diapir melting. Chemical Geology. 2025,695 :123065
[3] A stagnant subducted slab accelerates the deep Earth carbon cycle. Geology. 2025,53 :769–774
[4] Three-dimensional variations in carbon inputs to a subduction zone based on Mg–Zn isotopes. Geochimica et Cosmochimica Acta. 2025
[5] Trench-Perpendicular Mantle Flow Recorded by Late Mesozoic Intraplate Magmatism and Implications for the Formation of the Eastern Asian Big Mantle Wedge. Journal of Earth Science. 2025,36 (5):1879–1891
[6] Potassium isotopic evidence for recycling of surface water into the mantle transition zone. Nature Geoscience. 2024,17 :579–585
[7] Oligocene melting of subducted mélange and its mantle dynamics in northeast Asia. Geology. 2024,52 :539–544
[8] 东北亚陆缘晚白垩世岩浆作用对古太平洋俯冲作用变化的制约及其气候效应. 矿物岩石地球化学通报. 2023,65 (2):200-218
[9] Triggering of episodic back-arc extensions in the northeast Asian continental margin by deep mantle flow. Geology. 2023,51 (2):193–198
[10] Age, formation mechanisms, spatial extent, and geodynamic effects of the eastern and northeastern Asian big mantle wedges. Earth-Science Reviews. 2023,237 :104324
[11] Miocene transition from an active continental margin to a trench–arc–basin system in Northeast Asia: Constraints from compositional variations of basaltic rocks in the Russian Far East. Lithos. 2022,430-431 :106876
[12] High-latitude climatic response across the Triassic-Jurassic boundary recorded by Mg-Cu-Zn isotopes. Chemical Geology. 2022,610 :121085
[13] Geochronology and Sr-Nd-Pb-Hf isotopic geochemistry of middle-late Permian granitic and volcanic rocks within the eastern margin of the Khanka Massif: petrogenesis and implications for the tectonic nature. International Geology Review. 2022
[14] Transition from a passive to active continental margin setting for the NE Asian continental margin during the Mesozoic: Insights from the sedimentary formations and paleogeography of the eastern Jiamusi Massif, NE China. GEOLOGICAL SOCIETY OF AMERICA BULLETIN. 2022,134 (1–2):94–112
[15] Late Paleozoic–Mesozoic tectonic evolution of the northeastern Asian continental margin revealed by sedimentary formations and fossil accretionary complexes. Earth-Science Reviews. 2022,225 :103908

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