Lu Wang
State Key Lab for Geological Processes and Mineral Resources, and Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan 430074Songjie Wang
State Key Lab for Geological Processes and Mineral Resources, and Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan 430074Michael Brown
State Key Lab for Geological Processes and Mineral Resources, and Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan 430074；Laboratory for Crustal Petrology, Department of Geology, University Maryland, College Park, MD 20742, USABin Xia
State Key Lab for Geological Processes and Mineral Resources, and Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan 430074Timothy Kusky
State Key Lab for Geological Processes and Mineral Resources, and Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan 430074Ali Polat
State Key Lab for Geological Processes and Mineral Resources, and Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan 430074；3Department of Earth and Environmental Sciences, University of Windsor, Windsor, Ontario, Canada N9B 3P4P. Piccoli
Laboratory for Crustal Petrology, Department of Geology, University Maryland, College Park, MD 20742, USAT. Johnson
Department of Applied Geology, Curtin University, Perth, WA 6845, AustraliaLu Wang, Songjie Wang, Michael Brown, Bin Xia, Timothy Kusky, Ali Polat, P. Piccoli, T. Johnson.2018. Ten years of research progress on the structure, P–T path and Fluid–Melt evolution of the deeply-subducted UHP continental crust in the Sulu belt[J]. Acta Geologica Sinica(),92(z1):122-123
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