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    雪峰隆起西南缘下寒武统牛蹄塘组页岩气资源潜力评价

    Evaluation of Shale Gas Resource Potential in the Lower Cambrian Niutitang Formation at the Southwest Edge of Xuefeng Uplift

    • 摘要: 根据雪峰隆起西南缘下寒武统牛蹄塘组钻井及剖面资料,总结该区牛蹄塘组页岩气地质特征并开展有利区优选。研究结果表明:(1)研究区牛蹄塘组富有机质页岩沉积受深水陆棚环境控制,厚度由北西向南东逐渐增大;(2)牛蹄塘组富有机质页岩有机质丰度高,TOC平均值为4.95%;干酪根δ13C平均值为-33.04‰~-33.87‰,为Ⅰ型干酪根;有机质成熟度Ro多介于2.4%~2.6%之间,热演化程度适中;(3)牛蹄塘组石英矿物含量较高,储集空间主要为粒间孔、粒内孔、有机质孔和裂缝,孔隙度平均值为6.78%,渗透率平均值为0.0580×10-3μm2,属于低孔低渗-低孔超低渗储层;(4)利用多因素叠合法,优选出丹寨、宣威、麻江三个牛蹄塘组页岩气勘探有利区,地质资源量为3995.39×108m3

       

      Abstract: According to the drilling and profile data of the Lower Cambrian Niutitang Formation in the southwest margin of Xuefeng uplift, the geological characteristics of shale gas in the Niutitang Formation are summarized and the favorable areas are optimized. The research results show that:(1)The organic-rich shale deposits of Niutitang Formation in the study area are controlled by the deep-water shelf environment, and the thickness gradually increases from northwest to southeast.(2)The organic matter abundance of organic rich shale in the Niutitang Formation is high, with an average TOC of 4.95%; Cheese root δ The average value of 13C ranges from -33.04 ‰ to -33.87 ‰, indicating type I kerogen; The maturity of organic matter Ro is mostly between 2.4% and 2.6%, and the degree of thermal evolution is moderate.(3)The Niutitang Formation has a high content of quartz minerals, and the storage space is mainly composed of intergranular pores, intragranular pores, organic matter pores, and fractures. The average porosity is 6.78%, and the average permeability is 0.0580×10-3μm2 belongs to low porosity and low permeability - low porosity and ultra-low permeability reservoirs;(4)Using multiple factor superposition method, three favorable areas for shale gas exploration in the Niutitang Formation of Danzhai, Xuanwei, and Majiang were selected, with a geological resource of 3995.39×108m3.

       

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