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《Geochimica》 1998-06
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A STUDY ON THERMAL EVOLUTION OF JURASSIC SYSTEM,ERLIAN BASIN

Zhao Lin;Jia Rongfen; Qin Jianzhong; Guo Aiming ( Guangzhou Institute of Geochemistry, Chinese.Academy of Sciences, Guangzhou 510640)(Research Institute of Petroleum Exploration and Development,North China Administration, Renqiu 065502)  
Fission-track analysis, chemical kinetics model of vitrinite have been used to construct the thermal evolution of Jurassic System in Erlian Basin. The annealing depth of apatite from Drill hole Tucan 1 is 1600- 2587m, and the corresponding annealing paleotemperature is 64-102.7℃. The present temperature in the depth of the hole is lower than the highest palaeotemperature, because the palaeotemperature gradient dropped gradually, and the Jurassic System lifted and eroded. The highest temperature gradient which Jurassic System experienced is 7℃/ hm and 6.0℃ / hm,respectively according to simulation of fission-track analysis and chemical kinetics model of vitrinite. Jurassic System entered oil-generating stage in Late Cretaceous Period, and entered oil-generating peak in Tertiary Period.
【Fund】: 华北石油管理局横向课题!910407
【CateGory Index】: P618.130.2
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