A New Discovery of ～3.0 Ga Tonalitic Gneiss in Northern Liaoning Province, China  

作　　者：LI Zhuang LIU Jin WEI Chunjing CHEN Bin 

机构地区：[1]State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing) [2]College of Geosciences, China University of Petroleum (Beijing) [3]School of Earth Sciences and Engineering, Sun Yat-Sen University [4]School of Earth and Space Sciences, Peking University [5]School of Resources and Environmental Engineering, Hefei University of Technology

出　　处：《Acta Geologica Sinica(English Edition)》2018年第5期2043-2045,共3页地质学报（英文版）

基　　金：financially supported by the National Science Foundation of China(grants No.41430207 and 90914001)

摘　　要：Objective The North China Craton,bounded by the Paleozoic Central Asian Orogenic Belt on the north and by the Qinling–Dabie–Su–Lu Orogenic Belt on the south,is one of the oldest continental nuclei on Earth as a consequence of its preservation of some of the oldest rock records ranging up to ca.3.85 Ga and mineral older than 4.0 Ga（Li et al.,2016,2017）.Objective The North China Craton,bounded by the Paleozoic Central Asian Orogenic Belt on the north and by the Qinling–Dabie–Su–Lu Orogenic Belt on the south,is one of the oldest continental nuclei on Earth as a consequence of its preservation of some of the oldest rock records ranging up to ca.3.85 Ga and mineral older than 4.0 Ga（Li et al.,2016,2017）.

关 键 词：A New Discovery of ICP Pb China 

分 类 号：P588.345[天文地球—岩石学]