New Evidence of Detrital Zircon Ages for the Final Closure Time of the Paleo-Asian Ocean in the East

• 作 者: DU Qingxiang HAN Zuozhen SHEN Xiaoli HAN Chao SONG Zhigang GAO Lihua HAN Mei ZHONG Wenjian YAN Junlei
• 机 构: College of Earth Science and Engineering, Shandong University of Science and Technology,Shandong Pro
• 出 处: Acta Geologica Sinica(English Edition)
• 发表日期: 2017年05期

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,the timing of the

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, the timing of the