Neoarchaean-Palaeoproterozoic Mafic Dyke Swarms from the Singhbhum Granite Complex,Singhbhum Craton,Eastern India:Implications for Identification of Large Igneous Provinces and Their Possible Continuation on Other Formerly Adjacent Crustal Blocks  

作　　者：Rajesh K.Srivastava Ulf Soderlund Richard E.Ernst Sisir K.Mondal Amiya K.Samal 

机构地区：[1]Centre of Advanced Study in Geology,Institute of Science,Banaras Hindu University [2]Department of Geology,Lund University [3]Department of Earth Sciences,Carleton University [4]Faculty of Geology and Geography,Tomsk State University [5]Department of Geological Sciences,Jadavpur University

出　　处：《Acta Geologica Sinica(English Edition)》2016年第S1期17-18,共2页地质学报（英文版）

摘　　要：The Singhbhum craton of the eastern India consists of the Singhbhum Granite Complex(SGC)and the Chotanagpur Gneissic Complex(CGC)separated by the Singhbhum Mobile Belt(SMB).The CGC is intruded by Mesoproterozoic as well as Cretaceous mafic dykes;in

关 键 词：In Implications for Identification of Large Igneous Provinces and Their Possible Continuation on Other Formerly Adjacent Crustal Blocks Neoarchaean-Palaeoproterozoic Mafic Dyke Swarms from the Singhbhum Granite Complex Eastern India 

分 类 号：P588.1[天文地球—岩石学]