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Li Mingcheng(China University of Geosciences,Beijing,100083)  
Hot fluid activity within the crust is indeed the crustal fluidization,which is afrontier scientific subject emphasized and developed in the latest over ten years.Fluid is the most active geological agent within the crust where it can transmit energy and transfermaterial.Fluid action can affect and control directly tectonism,sedimentation,lithogene-sis,ore formation and other geological processes.The study on fluid action within thecrust may lead to the establishment of the completely new geoscience theory.Hydrocarbonmigration belongs to hot fluid activity occurred in the sedimentary basins,which runsthrough each stage of hydrocarbon generation,migration,accumulation and dissilation,controls directly the formation of hydrocarbon reservoirs,affects tectionic activities andlithogenesis in sedimentary basins,Research resluts of hydrocarbon migration can be usedfor reference in understanding the fluid activity of crust.Discontinuous episodic expulsionmechanism of hydrocarbons indicates metamorphic fluid activity in the deep parts of crustin episodic manner,produce episodic tectonic movements.Taking the action of deep fluidactivity into account,it is necessary to re-evaluate inorganic origin,thermal degradationabout hydrocarbon generation and hot watermigration of hydrocarbons in the deep parts ofbasin。
【Fund】: 国家“八五”攻关项目
【CateGory Index】: P618.130.1
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