姚玉来, 李士超, 杨建国, 肖飞, 李昂, 黄一鸣, 张渝金. 孙吴-嘉荫盆地东部太平林场组沉积相及烃源岩特征[J]. 地质与资源, 2023, 32(6): 713-719. DOI: 10.13686/j.cnki.dzyzy.2023.06.008
    引用本文: 姚玉来, 李士超, 杨建国, 肖飞, 李昂, 黄一鸣, 张渝金. 孙吴-嘉荫盆地东部太平林场组沉积相及烃源岩特征[J]. 地质与资源, 2023, 32(6): 713-719. DOI: 10.13686/j.cnki.dzyzy.2023.06.008
    YAO Yu-lai, LI Shi-chao, YANG Jian-guo, XIAO Fei, LI Ang, HUANG Yi-ming, ZHANG Yu-jin. SEDIMENTARY FACIES AND SOURCE ROCK CHARACTERISTICS OF TAIPINGLINCHANG FORMATION IN EASTERN SUNWU-JIAYIN BASIN[J]. Geology and Resources, 2023, 32(6): 713-719. DOI: 10.13686/j.cnki.dzyzy.2023.06.008
    Citation: YAO Yu-lai, LI Shi-chao, YANG Jian-guo, XIAO Fei, LI Ang, HUANG Yi-ming, ZHANG Yu-jin. SEDIMENTARY FACIES AND SOURCE ROCK CHARACTERISTICS OF TAIPINGLINCHANG FORMATION IN EASTERN SUNWU-JIAYIN BASIN[J]. Geology and Resources, 2023, 32(6): 713-719. DOI: 10.13686/j.cnki.dzyzy.2023.06.008

    孙吴-嘉荫盆地东部太平林场组沉积相及烃源岩特征

    SEDIMENTARY FACIES AND SOURCE ROCK CHARACTERISTICS OF TAIPINGLINCHANG FORMATION IN EASTERN SUNWU-JIAYIN BASIN

    • 摘要: 上白垩统太平林场组是孙吴-嘉荫盆地油气勘探重点层位. 通过野外详细的观测描述, 对盆地东部太平林场组剖面进行了沉积学研究. 结果表明太平林场组发育的沉积相类型为湖泊相和扇三角洲相, 可进一步划分出3种沉积亚相和6种沉积微相. 应用多种有机地球化学测试方法对太平林场组剖面泥页岩岩石学和有机地球化学特征进行分析, 结果显示泥页岩矿物成分以石英为主, 属于长英质泥页岩类; 显微组分以腐泥组为主, 具有倾油性; 烃源岩为中等-好烃源岩, 有机质类型为Ⅱ1-Ⅱ2型, 处于低成熟-成熟阶段. 表明太平林场组烃源岩具有较好的生烃潜力. 研究结果可为盆地后续深入研究和油气勘探提供基础资料.

       

      Abstract: The Upper Cretaceous Taipinglinchang Formation is the key oil-gas exploration horizon in Sunwu-Jiayin Basin. Based on the detailed field observation and description, the sedimentology of section of Taipinglinchang Formation in the east of the basin is studied in this paper. The results show that the sedimentary facies developed in Taipinglinchang Formation include lacustrine facies and fan delta facies, which can be further divided into 3 sedimentary subfacies with 6 sedimentary microfacies. The petrology and organic geochemical characteristics of the shale in Taipinglinchang Formation are analyzed by various organic geochemical testing methods. The results indicate that the mineral composition of shale is mainly quartz, belonging to felsic shale. The maceral composition is dominated by sapropelinite, with oil-prone property. The source rocks are of medium-good quality, with the organic matter types of Ⅱ1-Ⅱ2, which are in the low mature-mature stage, suggesting a good hydrocarbon potential. The results may provide basic data for further research and oil-gas exploration in the basin.

       

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