Tectonic Environments of the Yan-Liao Rift during Earth's Middle Age(1.7～0.75 Ga): Evidence from Mafic Dyke Swarms in Eastern Hebei, North China  

作　　者：WANG Chong PENG Peng WANG Xinping YANG Shuyan 

机构地区：[1]State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences [2]University of Chinese Academy of Sciences

出　　处：《Acta Geologica Sinica(English Edition)》2016年第S1期45-46,共2页地质学报（英文版）

基　　金：supported by the Major State Basic Research Development Program of China (973 Program; No: 2012CB416601);the National Natural Science Foundation of China (No: 41322018) projects;the National High-Level Talents Special Support Plan

摘　　要：During the past decade,generations of Precambrian mafic dykes/sills have been investigated and revealed in the North China Craton(NCC).Researchers identified more than 20 episodes of Precambrian dyke swarms,

关 键 词：North China Tectonic Environments of the Yan-Liao Rift during Earth’s Middle Age Evidence from Mafic Dyke Swarms in Eastern Hebei Ga 

分 类 号：P542[天文地球—构造地质学]