准噶尔盆地吉木萨尔凹陷二叠系芦草沟组不同岩相泥质烃源岩品质与含油性特征——以J10025井为例

Quality and oil-bearing properties of argillaceous hydrocarbon source rocks across different lithofacies of Permian Lucaogou Formation in Jimsar Sag, Junggar Basin: a case study of well J10025

  • 摘要: 不同岩相泥质烃源岩品质与含油性特征研究可为揭示页岩油富集规律及预测甜点提供重要依据。选取准噶尔盆地吉木萨尔凹陷J10025井二叠系芦草沟组57块泥岩样品,通过X射线衍射、薄片观察、岩石热解、有机岩石学、镜质体反射率、多温阶热解等综合分析,在岩相划分的基础上,系统研究了不同岩相泥质烃源岩品质与含油性特征。结果表明,吉木萨尔凹陷芦草沟组主要发育块状长英质泥岩、块状灰质泥岩、块状云质泥岩、纹层状长英质泥岩、纹层状含灰质泥岩、纹层状灰质泥岩和纹层状云质泥岩7类岩相。不同岩相泥质烃源岩品质差异明显,其中块状长英质泥岩和块状灰质泥岩品质较差,块状云质泥岩品质中等,纹层状长英质泥岩品质较好,而纹层状含灰质泥岩、纹层状灰质泥岩和纹层状云质泥岩为优质烃源岩。块状云质泥岩含油性和可动性相对较好,是相对有利的页岩油甜点岩相。J10025井大约在3 500~3 570 m和3 700~3 750 m深度区间存在含油性较好的泥岩,但整体可动性差,制约了泥岩类页岩油甜点的发育。影响泥岩含油性与可动性的主要因素包括生烃能力、排烃效率与TOC含量。游离烃含量明显受控于泥岩的生烃能力,而泥岩普遍发生的高效排烃直接导致游离油含量减少;同时,高TOC含量导致大量吸附油的存在,制约了页岩油的可动性。

     

    Abstract: The study on the quality and oil-bearing properties of argillaceous hydrocarbon source rocks across different lithofacies is crucial for understanding shale oil enrichment patterns and predicting sweet spots. 57 mudstone samples from the Permian Lucaogou Formation in the well J10025 of the Jimsar Sag, Junggar Basin were selected in this study. Based on lithofacies classification, the quality and oil-bearing properties of those argillaceous hydrocarbon source rocks across different lithofacies were systematically investigated through X-ray diffraction (XRD), thin-section observation, rock pyrolysis, organic petrology, vitrinite reflectance (Ro) measurement, and multi-temperature pyrolysis. The results indicated that 7 lithofacies were predominantly developed in the Lucaogou Formation of the Jimsar Sag, including massive felsic mudstones, massive calcareous mudstones, massive dolomitic mudstones, laminated felsic mudstones, laminated calcareous-bearing mudstones, laminated calcareous mudstones, and laminated dolomitic mudstones. Distinct quality differences were observed in those source rocks. The massive felsic mudstones and massive calcareous mudstones exhibited poor quality, while massive dolomitic mudstones were moderate-quality source rocks. The laminated felsic mudstones demonstrated good quality, whereas laminated calcareous-bearing mudstones, laminated calcareous mudstones, and laminated dolomitic mudstones were high-quality hydrocarbon source rocks. The massive dolomitic mudstones exhibited relatively favorable oil-bearing capacity and mobility, making them potential sweet spot lithofacies. In the well J10025, mudstones with relatively good oil-bearing properties were deposited at depth intervals of approximately 3 500 to 3 570 m and 3 700 to 3 750 m. However, its overall poor mobility restricted the development of the mudstone-type shale oil sweet spots. The main factors influencing the oil-bearing capacity and mobility of mudstones included hydrocarbon-generating capacity, hydrocarbon expulsion efficiency, and total organic carbon (TOC) content. The content of free hydrocarbons was significantly controlled by the hydrocarbon-generating capacity of mudstones. Meanwhile, the widespread efficient hydrocarbon expulsion in mudstones directly led to a reduction of free oil content. Additionally, high TOC content resulted in a large amount of adsorbed oil, which constrained shale oil mobility.

     

/

返回文章
返回