Neoproterozoic Magmatism in the Northern Margin of the Tarim Craton: Implications for Rodinia Reconstruction  

作　　者：ZHANG Zhaowei TANG Qingyan LI Chusi WANG Yalei 

机构地区：[1]MLR Key Laboratory for the study of Focused Magmatism and Giant Ore Deposits, Xi'an Institute of Geology and Mineral Resources [2]School of Earth Sciences and Key Laboratory of Mineral Resources in Western China (Gansu Province), Lanzhou University [3]Department of Geological Sciences, Indiana University

出　　处：《Acta Geologica Sinica(English Edition)》2016年第S1期171-,共1页地质学报（英文版）

基　　金：financially supported by the Special Fund for the Land and Resources Scientific Research of Public Interest (201511020)

摘　　要：The geodynamic processes for the Neoproterozoic mafic-ultramafic intrusions and dykes in the Kuluketage region,Tarim Craton has also been debated for some time.Some researchers suggested that the Neoproterozoic

关 键 词：Neoproterozoic Magmatism in the Northern Margin of the Tarim Craton Implications for Rodinia Reconstruction 

分 类 号：P588.1[天文地球—岩石学] P542[天文地球—地质学]