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《Acta Scicentiarum Naturalum Universitis Pekinesis》 2004-02
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Analysis on Tectonic Setting and Exhumation of Hengshan HP-Granulites

ZHANG Zhiqiang LI Jianghai HUANG Xiongnan NIU Xianglong (Department of Geology, School of Earth and Space Sciences,Peking University,Beijing,100871)  
HP(high pressure)-granulites are very important for understanding compositions of lower continental crust and tectonism.A neoarchean tectonic model of the North China is built by analysing on setting and exhumation of Hengshan HP-granulites, correlation between Hengshan metamorphic terrain and Wutai metamorphic terrain.The studies of p-T-t path the HP granulites show that it experienced p and T increasing during the subduction of the continental crust at first,and then,uplift in a way of clockwise ITD and cooling in a way of IBC,and finally exhumed.The studies of geological relations between Hengshan metamorphic terrain and Wutai metamorphic terrain confirm that they were actually the coupled and represented the island-arc root zone and shallow crust respectively.There are many kinds of conglomerates in Wutai foreland basin.Many evidences show age of Wutai foreland basin is 2.5?Ga.It is suggested that HP-granulites and Wutai foreland basin were formed during a “Andes type” subduction-collision.The western block collision with the eastern block occurred at 2.5?Ga.
【Fund】: 国家自然科学基金 (4 0 2 4 2 0 1 4 ;4 9832 0 30 );; 北京大学 985基金资助项目
【CateGory Index】: P588.3
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