source rock evaluation,oil source correlation,geochemistry,Zaoyuan exploration area,Yanchang Formation,Ordos basin ,"/> <p class="MsoPlainText"> 鄂尔多斯盆地枣园探区延长组长7段和长9段烃源岩评价及油源对比

吉林大学学报(地球科学版) ›› 2022, Vol. 52 ›› Issue (3): 840-854 .doi: 10.13278/j.cnki.jjuese.20210116

• 地质与资源 • 上一篇    下一篇

鄂尔多斯盆地枣园探区延长组长7段和长9段烃源岩评价及油源对比

王晓琳1,张小莉1,王祥1,曹聪2   

  1. 1.西北大学地质学系/大陆动力学国家重点实验室/二氧化碳捕集与封存技术国家地方联合工程研究中心,西安710069

    2.西安石油大学地球科学与工程学院,西安710065

  • 出版日期:2022-05-26 发布日期:2024-01-03
  • 基金资助:

    国家油气重大专项项目(2017ZX05005-002-004);国家科技重大专项(2016ZX05002-005-001)

Source Rocks Evaluation and Resource Potential Analysis of Chang 7 Member and Chang 9 Member of Yanchang Formation in Zaoyuan Exploration Area, Ordos Basin

Wang Xiaolin1, Zhang Xiaoli1, Wang Xiang1, Cao Cong2   

  1. 1. Department of Geology/State Key Laboratory of Continental Dynamics/National Local Joint Engineering Research Center

    for Carbon Dioxide Capture and Storage Technology, Northwest University, Xi’an 710069, China

    2. School of Earth Science and Engineering, Xi’an University of Petroleum, Xi’an 710065, China

  • Online:2022-05-26 Published:2024-01-03
  • Supported by:
    Supported by the National Oil and Gas Major Project (2017ZX05005-002-004) and the National Science and Technology Major Project (2016ZX05002-005-001)

摘要:

运用现代地球化学分析测试和生物标志化合物分析方法,研究了鄂尔多斯盆地枣园探区延长组长7、长9段烃源岩特征,并针对长4+5、长61和长8段的原油样品进行了地球化学分析和油源对比研究。结果表明:研究区长7段烃源岩有机质丰度较高,有机质类型主要为Ⅱ1-Ⅱ2型,规则甾烷C27-C28-C29构型为“V”字型或偏“V”字型,为湖相腐泥特征,长9段烃源岩有机质丰度较低,有机质类型为Ⅱ2型,规则甾烷C27-C28-C29构型为“L”型,与陆相高等植物混入密切相关;长4+5、长61和长8段的原油Pr/Ph值介于0.78~0.85之间,说明其沉积环境属于淡水还原环境;长4+5段原油与长61段原油相似,且来自于同一套陆相淡水湖泊烃源岩,属于中等—偏低成熟原油,长8段原油比长4+5、长61段原油成熟度高;延长组长4+5、长61、长8油层原油主要来自于长7段暗色泥页岩,长9段暗色泥页岩也可提供少量烃源。


关键词: 烃源岩评价, 油源对比, 地球化学, 枣园探区, 延长组, 鄂尔多斯盆地

Abstract: Modern geochemical analysis and biomarker analysis methods, the characteristics of Chang 7 Member and Chang 9 Member source rocks in Zaoyuan exploration area of Ordos basin were studied, and oil source correlation of Chang 4+5 Member Chang 61 Member and Chang 8 Member crude oil samples were carried out. The results show that the organic matter abundance of the source rocks of Chang 7 Member in the study area is higher, the type of organic matter is Ⅱ1-Ⅱ2, and the configuration of regular sterane C27-C28-C29 is V-shaped or partially V-shaped, which is the characteristic of sapropel; The organic matter abundance of Chang 9 Member source rocks is lower, the type of organic matter is Ⅱ2, and the configuration of regular sterane C27-C28-C29 is L-shaped, which is the characteristic of close mixing with terrestrial higher plants. The results show that the crude oil Pr/Ph ratios of Chang 4+5 Member, Chang 61 Member and Chang 8 Member are between 0.78 and 0.85, which indicate that their sedimentary environment belongs to a freshwater reducing environment; The crude oil of Chang 4+5 Member, Chang 61 Member and Chang 8 Member come from the same set of continental freshwater lake source rocks similar to Chang 61 Member, belonging to medium low mature crude oil. The crude oil of Chang 8 Member is more mature than that of Chang 4+5 Member and Chang 61 Member. The crude oil of Chang 4+5 Member, Chang 6 Member and Chang 8 Member in Zaoyuan exploration area is mainly from the dark mudstones, the main contributor is the Zhangjiatan shale of Chang 7 Member, and the dark mudstone of Chang 9 Member also makes a small contribution. 

Key words: source rock evaluation')">

source rock evaluation, oil source correlation, geochemistry, Zaoyuan exploration area, Yanchang Formation, Ordos basin

中图分类号: 

  • P59
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