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《Earthquake Research In Shanxi》 2002-04
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Deep-seated Tectonics in the North China Intraplate

XING Ji shan 1,LIU Jian hua 2,ZHAO Jin quan 3 (1 Geological Survey of Shanxi Province,Shanxi,Yuncheng 044004,China; 2 Geology and Geophysics Institute of Scientific Academy of China,Beijing 100101,China; 3 Seismological Bureau of Shanxi Prov  
main developing periods,which are early Precambrian periodin,Yenshan and Himalaya epochs come through in the formation of the North China plate.Many special tectonic blocks in the intraplate in Mesozoic and Neozoic era were formed,due to the movement of the North China plate itself,stress field acted on it as well as heterogeneity of the lithosphere of the upper mantle.a study on deep seated structure of the North China intraplate is made,by comprehensively using the results from geology,geophysics and geochemistry.Base on the deep seated tectonics,6 gold multi metal and 4 diamond mineral formation zones are mapped out.Also,some discussions on the relation between earthquakesas well as geothermal resource and the continental rift in the Neozoic era aremade.
【CateGory Index】: P315.2
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