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Petrogenic Indicator of Zedang Mantle Peridotite, Tibet: Insights from the Unusual Minerals

Petrogenic Indicator of Zedang Mantle Peridotite, Tibet: Insights from the Unusual Minerals

作     者:GUO Guolin YANG Jingsui LIU Xiaodong XU Xiangzhen ZHANG Zhongming TIANYazhou XIONG Fahui WU Yong 

作者机构:CARMA State Key Laboratory of Continental Tectonic and Dynamics Institute of Geology Chinese Academy ofGeological Sciences Beijing 10003 7 China Fundamental Science on Radioactive Geology and Exploration Technology Laboratory East China Institute ofTechnology Nanchang Jiangxi 330013 China 

出 版 物:《Acta Geologica Sinica(English Edition)》 (地质学报(英文版))

年 卷 期:2015年第89卷第A02期

页      面:20-21页

核心收录:

学科分类:0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学] 

基  金:financially supported by the National Natural Science Foundation of China (40930313, 41262002) the Ministry of Science and Technology of China (2014DFR21270) China Geological Survey (12120115026801, 12120115027201, 201511022) the Fund from the State Key Laboratory of Continental Tectonics and Dynamics (Z1301-a20) 

主  题:PETROGENESIS RESEARCH PERIDOTITE MINERALS MINERALOGY EARTH'S mantle 

摘      要:Resent studies show that a large number of unusual minerals are hosted mainly by chromites in the mantle sections of ophiolites (Bai et al., 2000;Yang et al., 2007; Yang et al., 2015). These minerals include native elements, oxides, carbides, PGE and base metal alloys, sulphides, silicates and have significant potential petrogenic and geodynamic significance.

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