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[1] 吉林敦化地区万宝岩组碎屑锆石U-Pb-Hf同位素组成:对区域构造演化的制约. 吉林大学学报(地球科学版). 2024,54 :1264-1279
[2] Subduction history of the paleo-Asian oceanic slab along the northern margin of the North China Craton; a case study of zircons and cherts from central Jilin Province, NE China. Geological Society of America bulletin. 2024,136
[3] Two distinct early Paleozoic subduction zones in the eastern Central Asian Orogenic Belt: Evidence of subduction recycling and arc evolution. Gondwana Research. 2024,134 :326-346
[4] Early Carboniferous seafloor spreading recorded by volcanic rocks in the western segment of the Changchun–Yanji Suture Belt, NE China. Geological Journal. 2020
[5] 延边开山屯地区二叠纪地质体的构造属性：侵入岩及碎屑锆石证据. 岩石学报. 2020,36 :759-780
[6] Supra-subduction zone ophiolite generated by the initial subduction of an Early Paleozoic island arc system abutting the northern North China Craton: Evidence from meta-igneous rocks. Gondwana Research. 2022,110 :90-106
[7] Petrogenesis of Early Mesozoic volcanic rocks in southeastern NE China: Geochemical and Sr–Nd–Pb–O isotopic evidences. Lithos. 2023,436-437
[8] Petrogenesis of Early Cretaceous volcanic rocks of the northeastern North China Craton: Constraints from elemental and Sr–Nd–Pb isotope geochemistry. Lithos. 2021,392-393
[9] Detrital Zircon U-Pb Geochronology of the Xilin Group: Constraints for the Early Paleozoic Tectonic Evolution of the Songliao Massif. Acta Geologica Sinica (English Edition). 2021,95 (6):2063-2074
[10] 鲁西费县中生代玄武岩及幔源捕掳晶的矿物化学:对岩石圈地幔性质的制约. 高校地质学报. 2004,10 (1)
[11] 华北克拉通东北缘岩石圈深部物质组成的不均一性：来自吉林南部中生代火山岩元素及Sr-Nd同位素地球化学的证据. 岩石学报. 2009,25 (08):1962-1974
[12] 吉南—辽南中生代镁铁—超镁铁质岩石的年代学及地球化学：对华北克拉通破坏空间范围的制约. Journal of Asian Earth Sciences. 2011,40 (2):636-650
[13] 吉林通化赤柏松辉长岩锆石SHRIMP U-Pb定年及其地质意义. 科学通报. 2005,49 (4):393-398
[14] 松辽盆地基底变质岩的锆石U-Pb年代学. 科学通报. 2007,52 (7):942-948
[15] 中国东北地区吉南晚中生代花岗岩的成因：地质年代学、地球化学和Sr-Nd-Hf同位素证据. Lithos. 2011,125 (1-2):27-39

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