机译:Early Cretaceous (~138-134 Ma) Forearc Ophiolite and Tectonomagmatic Patterns in Central Tibet: Subduction Termination and Re-initiation of Meso-Tethys Ocean Caused by Collision of an Oceanic Plateau at the Continental Margin?
China Univ Geosci, Sch Earth Sci & Resources, Beijing, Peoples R China|China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing, Peoples R China;
Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou, Peoples R China|CAS Ctr Liicellence Deep Earth Sci, Guangzhou, Peoples R China;
CAS Ctr Liicellence Deep Earth Sci, Guangzhou, Peoples R China|China Geol Survey, Beijing, Peoples R China|China Geol Survey, Remote Sensing Ctr Nat Resources, Beijing, Peoples R China|China Geol Survey, Chengdu Ctr, Chengdu, Peoples R China;
central Tibet; fore; 8208; arc spreading; Oceanic plateau; Ophiolite; Magmatic lull; Tethys Ocean;