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Petroleum geochemistry and origin of shallow-buried saline lacustrine oils in the slope zone of the Mahu sag, Junggar Basin, NW China

引用

Petroleum Science 2023年第6期20卷 3363-3378页

作者： Dong-Yong Wang Mei-Jun Li Yang Zhou Lu Yang Yuan-Feng Yang Er-Ting Li Jun Jin Xian-Li Zou Bo-Dong Xu State Key Laboratory of Petroleum Resources and Prospecting China University of Petroleum(Beijing)Beijing102249China College of Geosciences China University of Petroleum(Beijing)Beijing102249China College of Chemistry and Environmental Engineering Sichuan University of Science and EngineeringZigong643000SichuanChina College of Resources and Environment Chengdu University of Information TechnologyChengdu610225SichuanChina Baikouquan Oil Production Plant Xinjiang Oilfield Company CNPCKaramay834000XinjiangChina Research Institute of Experiment and Detection of Xinjiang Oilfield Company CNPC Karamay834000XinjiangChina Faculty of Petroleum China University of Petroleum(Beijing)at KaramayKaramay834000XinjiangChina

Recently, significant oil discoveries have been made in the shallower pay zones of the Jurassic Badaowan Formation (J_(1)b) in the Mahu Sag, Junggar Basin, Northwest China. However, little work has been done on the geochemical characteristics and origins of the oil in the J_(1)b reservoir. This study analyzes 44 oil and 14 source rock samples from the area in order to reveal their organic geochemical characteristics and the origins of the oils. The J_(1)b oils are characterized by a low Pr/Ph ratio and high β-carotene and gammacerane indices, which indicate that they were mainly generated from source rocks deposited in a hypersaline environment. The oils are also extremely enhanced in C_(29) regular steranes, possibly derived from halophilic algae. Oil-source correlation shows that the oils were derived from the Lower Permian Fengcheng Formation (P_(1)f) source rocks, which were deposited in a strongly stratified and highly saline water column with a predominance of algal/bacterial input in the organic matter. The source rocks of the Middle Permian lower-Wuerhe Formation (P_(2)w), which were deposited in fresh to slightly saline water conditions with a greater input of terrigenous organic matter, make only a minor contribution to the J_(1)b oils. The reconstruction of the oil accumulation process shows that the J_(1)b oil reservoir may have been twice charged during Late Jurassic–Early Cretaceous and the Paleogene–Neogene, respectively. A large amount volume of hydrocarbons generated in the P_(1)f source rock and leaked from T_(1)b oil reservoirs migrated along faults connecting source beds and shallow-buried secondary faults into Jurassic traps, resulting in large-scale accumulations in J_(1)b. These results are crucial for understanding the petroleum system of the Mahu Sag and will provide valuable guidance for petroleum exploration in the shallower formations in the slope area of the sag.

关键词： Molecular marker Saline lacustrine oil Petroleum origin Lower Permian Fengcheng Formation shallow-buried reservoir Mahu Sag

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