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《Journal of Changchun University of Science and Technology》 2004-01
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Researches of thermal evolution history in Hailaer basin

CHEN Shou-tian~(1,2), LIU Zhao-jun~(3), YU Hong-jin~(2) (1.Basin and Reservior Research Center,University of Petroleum,Beijing102249,China;2.Daqing Petroleum Administration, Daqing163412,China;3.College of Earth Sciences,Jilin University,Changchun130026,China)  
Hailaer basin is characterized by middle geotemperature and middle on lower terrestrial host flow. Vitrinite reflectance rises with increase of buried depth. The thermal evolution of source rock is different in different horizon and depression. Vitrinite reflectance is the greastest in Wuerxun and Beier depression, the degree of thermal evolution is the highest. Based on vitrinite reflectance,palaeogeotemperature and palaeogeothermal gradient are evaluated, palaeogeotemperature is higher than present geotemperature in Hailaer basin. Geothermal gradient was higher before Nantun Formation was deposited, it is (4.0~5.8)×10~(-2)℃/m.Palaeogeothermal gradient is higher in Wuerxun and Beier depressions, and oil-producing threshold is shallow, which is of advantage to formation oil and gas. Oil-producing threshold is deep in other depressions, it is of disadvantage to formation oil and gas.
【Fund】: 中国石油天然气集团公司资助项目(2002404-02)
【CateGory Index】: P314
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