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Plate divergent-convergent coupling system and dynamic mechanism of continental orogenic belts

作     者:Wenjiao XIAO 

作者机构:Xinjiang Institute of Ecology and GeographyChinese Academy of SciencesUrumqi 830011China 

出 版 物:《Science China Earth Sciences》 (中国科学(地球科学英文版))

年 卷 期:2023年第66卷第8期

页      面:1909-1912页

核心收录:

学科分类:070904[理学-构造地质学] 0709[理学-地质学] 07[理学] 

主  题:tectonics continental orogenic 

摘      要:Since the establishment of the theory of plate tectonics in the1960s and 1970s,the comprehension of global tectonics has shifted from “fixism to “mobilism,which is hailed as a revolution in earth science(Vine,1966;Dewey and Bird,1970).According to the basic theoretical framework of plate tectonics,the Earth’s surface can be divided into a number of rigid lithospheric plates,which move relative to one another on the ductile asthenosphere,giving rise to deformation。

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