Intra-Oceanic Subduction Termination and Reinitiation of the Eastern Neo-Tethys in Myanmar  

作　　者：Yi Chen Qinghua Zhang Lin Chen Kaihui Shi Kyaing Sein 

机构地区：[1]State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China [2]University of Chinese Academy of Sciences,Beijing 100049,China [3]Myanmar Geosciences Society,Hlaing University Campus,Yangon 11062,Myanmar

出　　处：《Journal of Earth Science》2024年第3期1053-1058,共6页地球科学学刊（英文版）

基　　金：supported by the National Natural Science Foundation of China(No.42172064)。

摘　　要：Subduction initiation and termination represent the birth and death of a subduction zone and are inevitable elements of terrestrial plate tectonics.Increasing evidence demonstrates that subduction zone processes did not operate continuously and might involve multiple initiation and termination stages(Stern,2004),characterized by sustained subduction-zone death and rebirth.Many geological and numerical studies focus on subduction initiation processes/mechanisms(see reviews in Yang,2022);however,subduction termination is often studied numerically at continental margins(Gerya,2022).How subduction termination proceeds in intra-oceanic settings remains enigmatic due to lacking geological records.

关 键 词：Eastern TERRESTRIAL CONTINENTAL 

分 类 号：P54[天文地球—构造地质学]