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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2006-06
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A research on the paleotemperature recovery and thermal evolution history of the Yining subbasin,Xinjiang,China

WANG Jun~1,LIU Jia-duo~1,TIAN Jing-chun~1,HOU Zhi-jiang~21.Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu 610059,China;2.Scientific Research Institute of Exploration and Development,Zhongyuan Oilfield Company ofSINOPEC,Puyang 457001,China  
This paper recovers the paleotemperature evolution history of the Yining sub-basin based on the thermometric data of the secondary fluid inclusions in quartz from Well Ning 3 and by Easy-R_o method used in multiple wells.The result shows that the geothermal gradient of the Yining sub-basin in Late Permian was 40℃/km,then it experienced two fluctuations(in K_1 and E_1 structural movements respondingly) and decreased to the present 24℃/km.This paper also recovers the thermal evolution history of the Yining sub-basin by basin modeling and combining with the thermal evolution features of source rocks.The evolution history suggests that the thermal evolution degree in Upper Permian was mainly controlled by paleotemperature,and the oil generating period was in Middle and Late Triassic.Traps formed before Indo-Chinese epoch was the principle hydrocarbon accumulation of Permian.
【CateGory Index】: P618.13
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