Newly Discovered Ca. 163 Ma OIB-Type Diabase Dike from the Shiquanhe Ophiolites, Western Tibet  

作　　者：LI Chenwei LI Zhijun CAO Hui ZENG Min 

机构地区：[1]State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation and College of Earth Sciences,Chengdu University of Technology [2]Institute of Geology,Chinese Academy of Geological Sciences

出　　处：《Acta Geologica Sinica(English Edition)》2018年第6期2443-2444,共2页地质学报（英文版）

基　　金：financially supported by the National Natural Science Foundation (grants No. 41102065 and 41872110);the Sichuan Science and Technology Program (grant No. 2018JY0465)

摘　　要：Objective The Shiquanhe ophiolite is an important tectonic belt in western Tibet. It has been debated whether the Shiquanhe ophiolite represents an allochthonous nappe derived from the Bangong-Nujiang suture zone to the north or the

关 键 词：OIB Th Pb Ma OIB-Type Diabase Dike from the Shiquanhe Ophiolites Newly Discovered Ca 

分 类 号：P[天文地球]