塔里木盆地西北缘奥陶系萨尔干组与印干组烃源岩特征对比及生烃潜力评价

    Comparison of source rock characteristics between the Ordovician Saergan Formation and Yingan Formation in the northwestern margin of Tarim Basin and their hydrocarbon generation potential evaluation

    • 摘要: 萨尔干组与印干组是塔里木盆地奥陶系两套重要的海相烃源岩,虽然两套地层均发育于较深水的沉积环境,但在有机质丰度、类型及富集机制方面存在差异。基于塔里木盆地西北缘柯坪地区的露头和地震资料,综合运用有机地球化学和沉积学方法,系统剖析两套烃源岩的沉积特征及生烃潜力。研究结果表明: 萨尔干组形成于中—晚奥陶世,与该时期的缺氧事件有关,以黑色页岩为主,总有机碳(total organic carbon,TOC)平均含量为1.88%,最高可达5.50%,有机质类型为II型,处于高成熟-过成熟阶段,生烃潜力巨大; 印干组形成于晚奥陶世,以深灰色-灰黑色泥岩、页岩为主,TOC平均含量仅为0.45%,有机质丰度较低,处于成熟-高成熟阶段。两套烃源岩的差异主要来源于古生产力与保存条件的不同,萨尔干组受控于缺氧事件引发的高古生产力与高埋藏效率,而印干组虽然处于缺氧环境,但古生产力水平较低。研究成果揭示了构造-沉积背景对海相烃源岩发育的控制机制,明确了全球性大洋缺氧事件与区域构造活动在烃源岩形成中的不同作用,可为塔里木盆地奥陶系油气勘探目标优选和资源潜力评价提供地质依据,对指导深层海相油气勘探具有实践意义。

       

      Abstract: Saergan Formation and Yingan Formation are two important marine hydrocarbon source rock units within the Ordovician System of Tarim Basin. Both of these two formations were developed in deep-water sedimentary environments, but they exhibited differences in organic matter abundance, type, and enrichment mechanisms. Based on the outcrop and seismic data from Kalpin area in the northwestern margin of Tarim Basin, the authors in this paper systematically analyzed the sedimentary characteristics and hydrocarbon generation potential of these two source rock units by comprehensively applying organic geochemical and sedimentological methods. The research results showed that Saergan Formation was formed during the Middle to Late Ordovician, associated with anoxic events of that period. The black shale was the major strata and the average total organic carbon (TOC) content was 1.88%, reaching a maximum of 5.50%. The kerogen was in Type II, which was at high maturity-overmature stage, demonstrating enormous hydrocarbon generation potential. Yingan Formation formed in the Late Ordovician, mainly consisting of dark gray to gray-black mudstone and shale. The average TOC was only 0.45% and the organic matter abundance was low, indicating maturity-high maturity stage. The differences between these two source rock units were primarily from variations in paleoproductivity and preservation conditions. Saergan Formation was controlled by high paleoproductivity and high burial efficiency triggered by anoxic events, whereas Yingan Formation was in an anaerobic environment with relatively low paleoproductivity levels. This study not only revealed the controlling mechanisms of tectonic-sedimentary background on the development of marine source rocks, but also clarified the different roles of global oceanic anoxic events and regional tectonic activities in source rock formation. This study could provide important geological evidence for optimizing oil and gas exploration targets and evaluating resource potential in the Ordovician of Tarim Basin, offering practical implications for guiding deep marine oil and gas exploration.

       

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