Geochemistry and Geochronology of the High-Mg Gabbro Dykes from Quanji Massif: Implications for the Amalgamation of Tarim Block in NW China and Assembly of the Rodinia Supercontinent

作     者：LIAO Fanxi CHEN Nengsong M.Santosh SUN Min WANG Qinyan XU Yixian 

作者机构：International Research Centre for Geology and Resources along the Silk Roads China University of Geosciences Faculty of Earth Science China University of Geosciences Journal Center China University of Geosciences Beijing Department of Earth Sciences The University of Hong Kong Institute of Geophysics and Geomatics China University of Geosciences 

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

年 卷 期：2016年第90卷第S1期

页      面：104-105页

核心收录：

学科分类：070904[理学-构造地质学] 070902[理学-地球化学] 0709[理学-地质学] 07[理学] 

基　　金：supported by the National Science Foundation of China (Nos. 41172069 and 41372075) the Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) 

主　　题：High-Mg gabbro dykes Geochemistry and geochronology Double-sided subduction Northwest China Supercontinent Rodinia 

摘      要：The Tarim Craton is one of the major continental blocks in *** dykes,ultra-mafic–mafic–carbonatite complex and ultra-mafic–mafic pluton of 0.82–0.75 Ga widely occur in Kuluktage,Aksu and Tieklik area along