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《EARTH SCIENCE FRONTIERS》 1995-04
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THE STUDY OF THE BASEMENT AND DEEP GEOLO-GICAL STRUCTURES OF SICHUAN BASIN,CHINA

Song Hongbiao;Luo Zhili(Chengdu Institute of Technology,Chengdu,610059)  
Based on regional geology,various geophysical surveys and deep well data,some new progresses about the deep structures of Sichuan basin have been acquired as fol-lows:Sichuan basin belongs to Yangtzi plate. Its lithosphere is greatly thick.In someplaces its thickness may rise up to 200km. The plateau of western Sichuan belongs to theeastern Tibet-Qinghai plate,it is located at the middle section of structural belt of Chi-na. Below its lithosphere,the asthenosphere has been uplifted in NE direction and thelithosphere becomes thinner with the least thickness being about 70km.The basement ofSichuan basin consists of crystalline basement and metamorphic sedimentary basement.The upper Sinian series is the first sedimentary capping bed in Sichuan basin after forma-tion of the ancient Yangtzi plate.The nature,thickness and depth of the basement are various within different sections of Sichuan basin,that makes thestructural division rec-ognizable.In addition,the basement faults impact the formation of basin and the develop-ment of cover greatly.
【Fund】: “八五”国家重点攻关项目,自然科学基金
【CateGory Index】: P542
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