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[1]Hongying Qu, Binwu Zhang, Miao Yu, Kurt Friehauf, Hui Wang, Chengyou Feng, Jeffrey M. Dick.Apatite as a record of ore-forming processes: Magmatic-hydrothermal evolution of the Hutouya Cu–Fe–Pb–Zn ore district in the Qiman Tagh Metallogenic Belt, NW China.Ore Geology Reviews, 2023, 154 (3-4) : 105343.
[2]于淼, 丰成友, 刘洪川, 李定武, 王辉, 刘建男, 赵一鸣, 李大新.青海尕林格矽卡岩铁多金属矿床Fe-Ti氧化物及其热动力学意义.地球学报, 2016, 37 (2) : 204-214.
[3]Uncovering chemical signatures of salinity gradients through compositional analysis of protein sequences.Biogeosciences Discussions, 2020, 146: 1-29.
[4]Geodynamic Setting and Cu-Ni Potential of Late Permian Xiwanggou Mafic-Ultramafic Rocks, East Kunlun Orogenic Belt, NW China.Frontiers in Earth Science, 2021, 9: 1-24.
[5]The tectonic evolution of the East Kunlun Orogen, northern Tibetan Plateau: a critical review with an integrated geodynamic model.Journal of Asian Earth Sciences, 191: 104168.
[6]Multistage amphiboles from the Galinge iron skarn deposit in Qiman Tagh, western China: evidence of igneous rocks replacement.Mineralogy and Petrology, 2017, 111 (1) : 81-97.
[7]Multistage skarn-related tourmaline from the Galinge deposit, Qiman Tagh, Western China: a fluid evolution perspective.The Canadian Mineralogist, 2017, 55 (1) : 3-19.
[8]Genesis of post-collisional calc-alkaline and alkaline granitoids in Qiman Tagh, East Kunlun, China.Lihtos, 2015, 239 (45-59)
[9]The Qiman Tagh Orogen as a window to the crustal evolution in northern Qinghai-Tibet Plateau.Earth-Science Reviews, 2017, 167 (103-123)
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