The Silurian A-Type Granites in Northeastern Guangxi,South China Block:New Evidence of Transition from Compression to Post-orogenic Extension of the Kwangsian Orogen

作     者：JIA Xiaohui WANG Xiaodi TANG Gongjian YANG Wenqiang NIU Zhijun 

作者机构：Wuhan Center of Geological SurveyChina Geological Survey State Key Laboratory of Isotope GeochemistryGuangzhou Institute of GeochemistryChinese Academy of Sciences 

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

年 卷 期：2016年第90卷第5期

页      面：1913-1914页

核心收录：

学科分类：070904[理学-构造地质学] 0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学] 

基　　金：supported by the National Science Foundation of China(grant No.41302046) China Geological Survey(grant No.12120113063600) 

主　　题：The Silurian A-Type Granites in Northeastern Guangxi South China Block 

摘      要：Objective More and more evidence suggests that the Kwangsian orogen is probably an intraplate orogen, which is one of the few examples of intraplate orogenesis worldwide. However, the initiation time, size and scope of the Kwangsian orogeny have not been determined yet. This study analyzed the Silurian A-type granites in northeastern Guangxi, South China Block, which may provide new evidence for the transition from compression to post- orogenic extension of the Kwangsian orogen.