Petrogenesis of the～2115 Ma Haicheng Mafic Sills in the Eastern North China Craton and Their Implications for An Intra-Continental Rifting  

作　　者：WANG Xinping PENG Peng WANG Chong YANG Shuyan 

机构地区：[1]State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences

出　　处：《Acta Geologica Sinica(English Edition)》2016年第S1期128-,共1页地质学报（英文版）

基　　金：supported by 973 (2012CB416601) and NFSC (41322018) projects

摘　　要：It is well known that there are widespread igneous events at;100 Ma in the Eastern North China Craton;however,their tectonic environments are controversial.They were thought to be either related to an intra-continental rifting or

关 键 词：Ma Haicheng Mafic Sills in the Eastern North China Craton and Their Implications for An Intra-Continental Rifting Petrogenesis of the 

分 类 号：P542[天文地球—构造地质学]