DEEP Neoarchean Subduction Indicated by Ultra-high Pressure TiO2 (II) Inclusion in Ophiolitic Podiform Chromitite Block in Mélange, Central (Taihang) Orogenic Belt, North China

Tim KUSKY1, *, WANG Lu1, Paul ROBINSON1, Richard WIRTH2 and HUANG Yang1

1 State Key Lab for Geological Processes and Mineral Resources, Center for Global Tectonics, China University of Geosciences, Wuhan 430074, China

2 Helmholtz Center Potsdam German Research Centre for Geosciences GFZ, D-14473 Potsdam, Germany

Citation: Kusky et al., 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. Acta Geologica Sinica (English Edition), 95(supp. 1): 85–87.

 KuskyAcademicaDEEPextendedabtract.pdf