Tim KUSKY
State Key Lab for Geological Processes and Mineral Resources, Center for Global Tectonics, China University of Geosciences, Wuhan 430074, ChinaWANG Lu
State Key Lab for Geological Processes and Mineral Resources, Center for Global Tectonics, China University of Geosciences, Wuhan 430074, ChinaPaul ROBINSON
State Key Lab for Geological Processes and Mineral Resources, Center for Global Tectonics, China University of Geosciences, Wuhan 430074, ChinaRichard WIRTH
Helmholtz Center Potsdam German Research Centre for Geosciences GFZ, D-14473 Potsdam, GermanyHUANG Yang
State Key Lab for Geological Processes and Mineral Resources, Center for Global Tectonics, China University of Geosciences, Wuhan 430074, ChinaTim KUSKY, WANG Lu, Paul ROBINSON, Richard WIRTH, HUANG Yang.2021. DEEP Neoarchean Subduction Indicated by Ultra-high Pressure TiO2 (II) Inclusion in Ophiolitic Podiform Chromitite Block in Mélange, Central (Taihang) Orogenic Belt, North China[J]. Acta Geologica Sinica(),95(z1):85-87
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