中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Evolution of the Pristane/Phytane Ratio with Maturity of Lacustrine Source Rocks: Implications of a Thermal Simulation Experiment

文献类型:期刊论文

作者Cheng, Peng; Gai, Haifeng; Xiao, Xianming; Zhou, Linyuan; Zhao, Wei; Zhou, Qin; Tian, Hui
刊名ACS EARTH AND SPACE CHEMISTRY
出版日期2023
卷号7期号:5页码:1072-1082
关键词RIVER MOUTH BASIN CRUDE OILS ORGANIC-MATTER GEOCHEMICAL CHARACTERISTICS DEPOSITIONAL-ENVIRONMENTS BIOLOGICAL MARKERS CHINA PHYTANE PETROLEUM HYDROCARBONS
ISSN号2472-3452
DOI10.1021/acsearthspacechem.3c00011
英文摘要The pristane/phytane ratio (Pr/Ph) of source rocks has been extensively used for the identification of paleosedimentary environments and oil-source rock correlations. However, the influences of maturity on the Pr/ Ph ratio are not fully understood, which largely limits the applicability of this parameter under geological conditions. Based on a thermal simulation experiment performed on typical lacustrine source rock samples and systematic research on geological source rock samples, the evolution of the Pr/Ph ratio with increasing maturity was investigated in this study. The results indicate that the Pr/Ph ratios of the two source rock extracts progressively decrease with increasing maturity, and the decrease in this parameter is more significant for shallow lacustrine samples than for deep lacustrine samples. The Pr/Ph ratios of the two types of source rocks are different at the oil generation stage with EasyRo less than 1.02% but are similar at the oil cracking stage with EasyRo larger than 1.02%. The Pr and Ph of source rocks are contributed by both biogenic and thermal origins, which are largely determined by the sedimentary environment and maturity, respectively, and the contributions of the two origins are diverse at different maturity stages. The Pr/Ph ratio is mainly controlled by the sedimentary environment at the diagenetic stage, by both sedimentary and thermal maturity at the oil generation stage, and by thermal maturity at the oil cracking stage. The Pr/Ph ratio of source rocks can be used to identify sedimentary environments and oil-source rock correlations at diagenetic and oil generation stages.
WOS研究方向Chemistry, Multidisciplinary ; Geochemistry & Geophysics
语种英语
WOS记录号WOS:000984856000001
源URL[http://ir.gig.ac.cn/handle/344008/80340]  
专题有机地球化学国家重点实验室
推荐引用方式
GB/T 7714
Cheng, Peng,Gai, Haifeng,Xiao, Xianming,et al. Evolution of the Pristane/Phytane Ratio with Maturity of Lacustrine Source Rocks: Implications of a Thermal Simulation Experiment[J]. ACS EARTH AND SPACE CHEMISTRY,2023,7(5):1072-1082.
APA Cheng, Peng.,Gai, Haifeng.,Xiao, Xianming.,Zhou, Linyuan.,Zhao, Wei.,...&Tian, Hui.(2023).Evolution of the Pristane/Phytane Ratio with Maturity of Lacustrine Source Rocks: Implications of a Thermal Simulation Experiment.ACS EARTH AND SPACE CHEMISTRY,7(5),1072-1082.
MLA Cheng, Peng,et al."Evolution of the Pristane/Phytane Ratio with Maturity of Lacustrine Source Rocks: Implications of a Thermal Simulation Experiment".ACS EARTH AND SPACE CHEMISTRY 7.5(2023):1072-1082.

入库方式: OAI收割

来源:广州地球化学研究所

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