Crustal growth and reworking at Archean plate margins  

作　　者：Xi WANG 

机构地区：[1]Frontiers Science Center for Deep Ocean Multispheres and Earth System,Key Lab of Submarine Geosciences and Prospecting Techniques,MOE,China,and College of Marine Geosciences,Ocean University of China,Qingdao 266100,China

出　　处：《Science China Earth Sciences》2023年第12期2977-2982,共6页中国科学（地球科学英文版）

基　　金：supported by the National Natural Science Foundation of China (Grant No.42072218)。

摘　　要：1.Introduction Archean cratons have attained and maintained long-term stability,and they are the main area for studying the geological processes and tectonic regime of early Earth.The majority of cratons have completed their cratonization through growth and assemblage of ancient continental nuclei in the late Archean(Cawood et al.,2018;Zeh and Kirchenbaur,2022).

关 键 词：ARCHEAN ASSEMBLAGE TECTONIC 

分 类 号：P542[天文地球—构造地质学] P534.2[天文地球—地质学]