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    桂中坳陷下石炭统鹿寨组页岩生烃潜力及有机—无机孔隙结构定量表征

    Quantitative characteristics of hydrocarbon generation potential and organic-inorganic pore structure of the Lower Carboniferous Luzhai Formation shale in the Guizhong Depression

    • 摘要:
      研究目的 桂中坳陷下石炭统鹿寨组页岩气资源潜力大,近年来取得了勘探突破,但其生烃潜力及有机—无机孔隙结构特征尚缺乏系统研究。
      研究方法 本文以鹿寨组一段1亚段页岩为研究对象,通过岩石热解分析、扫描电镜(SEM)孔隙提取与定量识别、氮气/二氧化碳吸附及高压压汞(MIP)定量表征等方法,在系统的页岩岩相类型划分基础上,对不同岩相页岩生烃潜力及有机—无机孔隙结构进行了定量表征,明确了鹿寨组优质页岩储层岩相类型。
      研究结果 结果表明,鹿寨组富有机质硅质岩相页岩具备良好的生烃潜力,其次是含有机质硅质页岩。鹿寨组页岩储层孔隙以微孔和中孔为主,孔隙类型主要包括有机孔、粒间孔、晶间孔及溶蚀孔,无机质孔隙是鹿寨组页岩储层孔隙空间最主要的贡献者。富有机质硅质页岩发育大量无机孔和微裂缝以及部分有机孔,储集能力最优;含有机质硅质页岩无机孔较发育,以及少量有机孔,储集潜力较强;含有机质灰质页岩和含有机质硅质混合质页岩孔隙连通性较差,储集能力相对较低。
      结论 综合分析认为,桂中坳陷鹿寨组富有机质硅质页岩生烃潜力高,储集能力好,是最有利的储层岩相类型,是页岩气勘探开发的优选岩相,成果为桂中坳陷鹿寨组页岩气高效勘探开发提供了理论支撑。

       

      Abstract:
      This paper is the result of oil and gas geological survey engineering.
      Objective The Lower Carboniferous Luzhai Formation in the Central Guangxi (Guizhong) Depression exhibits significant shale gas resource potential and has recently witnessed breakthroughs in shale gas exploration. However, systematic research on its hydrocarbon generation potential and organic-inorganic pore structure characteristics is still lacking.
      Methods This study focuses on the Sub-member 1 of the Luzhai Formation, based on a systematic classification of shale lithofacies types, the hydrocarbon generation potential and organic-inorganic pore structure of different lithofacies were quantitatively characterized, using methods including rock pyrolysis analysis, scanning electron microscopy (SEM) pore extraction and quantitative identification, nitrogen/carbon dioxide adsorption, and high-pressure mercury intrusion (MIP). This clarified the types of high-quality shale reservoirs in the Luzhai Formation.
      Results The results indicate that the organic-rich siliceous shale lithofacies within the Luzhai Formation possesses good hydrocarbon generation potential, followed by the organic-bearing siliceous shale lithofacies. The reservoir space of the shale is dominated by micropores and mesopores, with pore types mainly comprising organic pores, intergranular pores, intragranular pores, and dissolution pores. Inorganic pores are the primary contributors to the pore space in the Luzhai Formation shale reservoirs. The organic-rich siliceous shale, developing numerous inorganic pores, micro-fractures, and some organic pores, exhibits the optimal storage capacity. The organic-bearing siliceous shale, with well-developed inorganic pores and a small number of organic pores, shows strong storage potential. In contrast, the organic-bearing calcareous shale and organic-bearing siliceous mixed shale have poorer pore connectivity and relatively lower storage capacity.
      Conclusion Comprehensive analysis suggests that the organic-rich siliceous shale in the Luzhai Formation of the Central Guangxi Depression has high hydrocarbon generation potential and good storage capacity, making it the most favorable reservoir lithofacies type and the preferred target for shale gas exploration and development. These results provide theoretical support for the efficient exploration and development of shale gas in the Luzhai Formation within the Central Guangxi Depression.

       

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