Driving forces of continental lithospheric deformation  

作　　者：Zebin CAO Lijun LIU 

机构地区：[1]State Key Laboratory of Lithospheric and Environmental Coevolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China

出　　处：《Science China Earth Sciences》2024年第12期3950-3956,共7页中国科学（地球科学英文版）

基　　金：supported by the Strategy Priority Research Program(Category B)of the Chinese Academy of Sciences(Grant No.XDB0710000);the National Natural Science Foundation of China(Grant No.92355302)。

摘　　要：1.Introduction The lithosphere is a fundamental component of Earth’s layered structure,and its stress state and deformation mechanisms are critical to understanding Earth’s tectonic evolution(Ghosh and Holt,2012)and managing natural resources(Heidbach et al.,2018).According to the classical theory of plate tectonics,significant lithospheric deformation is expected near active plate boundaries due to the relative motion between tectonic plates.

关 键 词：TECTONIC LITHOSPHERIC EARTH 

分 类 号：P31[天文地球—固体地球物理学] P542[天文地球—地球物理学]