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《Journal of Changchun University of Science and Technology》 2002-04
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THE GENETIC TYPE OF THE MESOZOIC BASIN IN NORTHERN CHAIDAMU AND ITS TECTONIC-SEDIMENTARY EVOLUTION

HE Zhong hua,LIU Zhao jun,GUO Wei,DONG Qing shui (College of Earth Sciences,Jilin University,Changchun 130026,China)  
Chaidamu basin is a big MesoCenozoic oilbearing continental basin in NW China. Its section texture,structural style,sedimentary feature,basal subsidence and paleogeothermics show that the basin is a superimposed foreland basin related to Qilian orogenic belt during Meseozoic period,which was formed by episodic thrusting and evolved from early Jurassic broken foreland to the foreland like basin after middle Jurassic. Mesozoic sedimentary infills consist of three complete tectosequences,ie.,tectosequenceⅠ (early Jurassic),tectosequenceⅡ (middle Jurassic) and tectosequenceⅢ (late Jurassic). Sedimentary circles with the fining-upward trend indicate episodic thrusting from activity to quiescence. With strong and rapid thrusting,tectosequence Ⅳ(Cretaceous) only underwent active period and is not a complete tectosequence. At that time,the basin developed overfilled sediments and gradually withered.
【Fund】: 中国石油天然气集团公司“九五”科技工程资助项目 (QZ 972 0 4 10 2 )
【CateGory Index】: P544.4
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