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《Chinese Journal of Geophysics》 2005-01
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Apatite fission track evidence for the thermal history of the Liupanshan basin

ZHENG De-Wen, ZHANG Pei-Zhen, WAN Jing-Lin, YUAN Dao-Yang, ZHANG Guang-Liang, LI Chuan-You State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China  
Studying the thermal history of a basin will provide important constraints on determination of hydrocarbon generation and exploring target. Apatite fission track data suggest that the early Cretaceous strata in the Liupanshan basin were subjected to two burial heating events. The first heating event occurred during Cretaceous, and reached the maximum temperature prior to the end of Cretaceous. The second one occurred during Eocene-late Miocene, and reached the maximum temperature at about 8MaB.P. The first maximum temperature by burial heating is higher than the second one. The maximum temperature to which the Triassic-Jurassic hydrocarbon source rocks were subjected is higher than the oil generation peak phase. The Naijia River formation and the Madong Mountain formation were buried to the \!oil generation window" phase, but the maximum temperature is lower than the oil generation peak phase. According to the paleotemperature results, the Triassic-Jurassic strata may be the predominant hydrocarbon source rocks in the Liupanshan basin. The predominant hydrocarbon generation occurred prior to the end of Cretaceous.
【Fund】: 国家自然科学基金项目 (4 0 2 0 2 0 2 0 )和 (4 0 2 3 0 40 40 )资助
【CateGory Index】: P314
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