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《Acta Scicentiarum Naturalum Universitis Pekinesis》 2004-02
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Hot-Tectonic Events and Evolution of North Margin of the North China Craton in Meso-Neoproterozoic

ZHANG Chen (Department of Geology, School of Earth and Space Sciences, Peking University, Beijing, 100871)  
Up to date some studies proved that there are varieties of metamorphic sedimentary volcanic rocks, plutonic rocks and structural traces of Meso and Neoproterozoic along north margin of the North China craton. The tectonic history of Meso Neoproterozoic in the studied area could be summarized as follows: the extensional breaking in the early stage of the Meso Proterozoic, the compression convergencing in the late stage of the Meso Proterozoic, the extensional breaking in the early stage of the Neoproterozoic-Lower Paleozoic and the compression subducting in the late stage of the Lower Paleozoic.They are identified four stages representing the Meso and Neoproterozoic Paleozoic hot tectonical events and the ages obtained by analyzing the rock samples from north margin of the North China craton. The orogenic belt in late stage of the Meso Proterozoic along north margin of the North China craton, mainly consists of ophiolite relics of Kaiyuan rock group, island arc volcanic rocks of Weijiagou and Bainaimiao groups, and S type granites in the late stage of the Meso Proterozoic. The orogenic belt in late stage of the Meso Proterozoic along north margin of the North China craton related to other Meso Proterocoic orogenic belts on cratons of the world will provide important constraints for reconstructing the Rodinia super continent.
【Fund】: 国家自然科学基金资助项目 (4 0 0 72 0 72 )
【CateGory Index】: P542.2
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