New Evidence of Detrital Zircon Ages for the Final Closure Time of the Paleo-Asian Ocean in the Eastern Central Asian Orogenic Belt(NE China)  

作　　者：DU Qingxiang HAN Zuozhen SHEN Xiaoli HAN Chao SONG Zhigang GAO Lihua HAN Mei ZHONG Wenjian YAN Junlei 

机构地区：[1]College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, Shandong, China [2]Shandong Provincial Key Lab of Depositional Mineralization and Sedimentary Minerals, Shandong University of Science and Technology, Qingdao 266590, Shandong, China [3]Key Laboratory for Sedimentary Basin and Oil and Gas Resourcesy Ministry of Land and Resources, Qingdao 266590, Shandong, China

出　　处：《Acta Geologica Sinica(English Edition)》2017年第5期1910-1914,共5页地质学报（英文版）

基　　金：supported by the National Natural Science Foundation of China(grants No.41372108 and41602110);the Research Fund for the Doctoral Program of Higher Education of China(grant No.20133718130001);the Qingdao Postdoctoral Applied Research Project(grant No.2015193);the SDUST Research Fund(grant No.2015TDJH101)

摘　　要：Objective The NE China is located in the eastern segment of the Central Asian Orogenic Belt（CAOB）,which is a large accretionary orogen between the Siberian Craton and the North China Craton（NCC）.Many researches have discussed about the evolution of the Paleo-Asian Ocean（PAO）in the eastern CAOB.However,Objective The NE China is located in the eastern segment of the Central Asian Orogenic Belt（CAOB）,which is a large accretionary orogen between the Siberian Craton and the North China Craton（NCC）.Many researches have discussed about the evolution of the Paleo-Asian Ocean（PAO）in the eastern CAOB.However,

关 键 词：Th NE China New Evidence of Detrital Zircon Ages for the Final Closure Time of the Paleo-Asian Ocean in the Eastern Central Asian Orogenic Belt OHS NCC Pb 

分 类 号：P542.2[天文地球—构造地质学] P597.3[天文地球—地质学]