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准噶尔盆地沙湾凹陷二叠系下乌尔禾组烃源岩类型与热演化研究
引用本文:曾治平, 王金铎, 李超, 徐冰冰, 范婕, 刘德志, 李松涛, 张增宝. 2024. 准噶尔盆地沙湾凹陷二叠系下乌尔禾组烃源岩类型与热演化研究. 地质科学, 59(2): 330-340. doi: 10.12017/dzkx.2024.023
作者姓名:曾治平  王金铎  李超  徐冰冰  范婕  刘德志  李松涛  张增宝
作者单位:1. 中国石化胜利油田分公司勘探开发研究院 山东东营 257015; 2. 中国科学院地质与地球物理研究所 北京 100029; 3. 中国石化石油勘探开发研究院 北京 100083; 4. 中石化新疆新春石油开发有限责任公司 山东东营 257000
基金项目:中国石化科技部项目“准噶尔盆地腹部超深层P—T成储成藏机制及勘探方向”(编号:P22128)资助
摘    要:

沙湾凹陷下组合油气资源丰富,下乌尔禾组烃源岩被证实是凹陷内主要的油气来源。然而,由于烃源岩埋深较大、勘探程度低,烃源岩类型、热演化以及生烃史尚不清楚,制约了下组合油气成藏规律的认识。本研究基于烃源岩地球化学参数,认识下乌尔禾组烃源岩基本特征,利用盆地模拟恢复烃源岩热演化以及生烃演化史,在此基础上对油气成藏过程进行分析。结果表明:沙湾凹陷下乌尔禾组烃源岩有机质类型以Ⅱ型为主,平均有机碳含量(TOC)为0.82%,生烃潜量(S1+S2)为5.32 mg/g,为中等烃源岩,平均成熟度(Ro)为1.27%,处于成熟—高成熟阶段。热演化模拟显示下乌尔禾组烃源岩于晚三叠世晚期进入生烃门限(Ro=0.5%),晚侏罗世—晚白垩世达到生油高峰(Ro=1.0%)。白垩纪末期,有机质热演化进入了高成熟演化阶段(Ro>1.3%)。沙湾凹陷超深层储层经历多期油气充注,油气的多期混合以及断层活动的不均一性造成不同层位多种相态油气藏共存。研究认识为准噶尔盆地超深层油气成藏过程和机理研究奠定了坚实的基础。



关 键 词:烃源岩   热演化   生烃史   盆地模拟   沙湾凹陷
收稿时间:2023-09-13
修稿时间:2023-12-11

Research on the source rock types and thermal evolution of the Permian Lower Wuerhe Formation in the Shawan Sag,Junggar Basin
Zeng Zhiping, Wang Jinduo, Li Chao, Xu Bingbing, Fan Jie, Liu Dezhi, Li Songtao, Zhang Zengbao. 2024. Research on the source rock types and thermal evolution of the Permian Lower Wuerhe Formation in the Shawan Sag, Junggar Basin. Chinese Journal of Geology, 59(2): 330-340. doi: 10.12017/dzkx.2024.023
Authors:Zeng Zhiping  Wang Jinduo  Li Chao  Xu Bingbing  Fan Jie  Liu Dezhi  Li Songtao  Zhang Zengbao
Affiliation:1. Exploration and Development Research Institute, Shengli Oilfield Company, SINOPEC, Dongying, Shandong 257015; 2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029; 3. SINOPEC Petroleum Exploration and Production Research Institute, Beijing 100083; 4. Xinjiang Xinchun Petroleum Development Co., Ltd., SINOPEC, Dongying, Shandong 257000
Abstract:
The lower play in Shawan Sag is rich in oil and gas resources, and the Lower Wuerhe Formation has been proven to be the main source rock. However, the thermal evolution and hydrocarbon generation history of the source rock have not been clearly understood due to the deep burial and low research degree, which limits the understanding of the hydrocarbon migration and accumulation in lower play. Based on geochemistry data of source rock, the basic characteristic of the source rock is analyzed, and the thermal evolution and hydrocarbon generation history of the Lower Wuerhe Formation are reconstructed by basin modeling, and then the hydrocarbon accumulation process is preliminarily analyzed. The results show that the source rocks of the Lower Wuerhe Formation in the Shawan Sag are mainly Type Ⅱ organic matter, with an average organic carbon content of 0.82% and a potential hydrocarbon generation of 5.32 mg/g, which are medium source rocks. The current maturity is approximately 1.27% and they are in the mature to highly mature stage. The result of thermal evolution simulation shows that the source rocks entered the threshold of hydrocarbon generation(Ro = 0.5%)since the Late Triassic and reached the peak of oil generation (Ro = 1.0%) in the Jurassic-Late Cretaceous. After the end of the Cretaceous, the thermal evolution of organic matter entered a high maturity stage(Ro > 1.3%)and the kerogen was cracked to produce wet gas. The ultra-deep reservoir experiences multi-stage oil and gas charge, multi-stage mixed oil and gas charge and the fault differential activity result in the coexistence of multi-phase oil and gas reservoirs in different formations in the Shawan Sag. The research and understanding have established a strong basis for comprehending the mechanisms and procedures involved in the ultra-deep hydrocarbon accumulation within the Junggar Basin.
Keywords:Source rock  Thermal evolution  Hydrocarbon generation history  Basin modeling  Shawan Sag
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