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    桑琴, 未勇, 程超, 黄静, 吕宗刚, 吴昌龙, 彭祚远. 蜀南地区茅口组气藏气水分布特征及其控制因素[J]. 中国地质, 2012, 39(3): 634-644.
    引用本文: 桑琴, 未勇, 程超, 黄静, 吕宗刚, 吴昌龙, 彭祚远. 蜀南地区茅口组气藏气水分布特征及其控制因素[J]. 中国地质, 2012, 39(3): 634-644.
    SANG Qin, WEI Yong, CHENG Chao, HUANG Jing, LV Zong-gang, WU Chang-long, PENG Zuo-yuan. Gas-water distribution characteristics and control factors of Maokou Formation in Shunan (south Sichuan) area[J]. GEOLOGY IN CHINA, 2012, 39(3): 634-644.
    Citation: SANG Qin, WEI Yong, CHENG Chao, HUANG Jing, LV Zong-gang, WU Chang-long, PENG Zuo-yuan. Gas-water distribution characteristics and control factors of Maokou Formation in Shunan (south Sichuan) area[J]. GEOLOGY IN CHINA, 2012, 39(3): 634-644.

    蜀南地区茅口组气藏气水分布特征及其控制因素

    Gas-water distribution characteristics and control factors of Maokou Formation in Shunan (south Sichuan) area

    • 摘要: 提要:蜀南地区位于四川盆地南部,勘探面积为5.03×104 km2。该区茅口组为一套碳酸盐岩沉积,基质岩块具有低孔低渗的特征。在对工区地质、钻井、生产等资料分析和总结的基础上,对气水关系的复杂性进行了探讨,认为复杂的气水关系表现为:同一背斜构造范围内无统一的气水界面;同一缝洞系统也通常存在多个气水界面;一些缝洞系统在开发过程中经历了产纯气、气水同产、产纯气到再次气水同产等多个反复过程。根据气藏储层特征、开发动态和地层水演化分析,归纳出3种气水分布模式:似构造圈闭的整装气藏类型,背斜-缝洞复合圈闭类型,缝洞圈闭类型,并以宋家场、荔南桐、荷包场茅口组气藏为例加以说明。结合地质背景分析认为,不同的岩溶区域的水动力条件是控制气水分布的决定因素;构造运动控制了气水分布的调整;流体势特征指示了水体的活跃程度。

       

      Abstract: Abstract:Located in Sichuan basin, Shunan area has an exploration area of 5.03×104 km2. The Maokou Formation in this area is composed of carbonate rock with low porosity and low permeability. Based on a summary and analysis of the geological, drilling and production data, this paper deals with the complexity of gas-water distribution. There is no uniform gas-water interface in the same anticlinal structure, and many gas-water interfaces may exist in one fracture-cave system; the exploitation of some fracture-cave systems are characterized by the process from producing pure gas through producing gas and water to producing pure gas again. Based on an analysis of the reservoir characteristics, the exploitation dynamic state and the evolution of the formation water, the authors formulated three gas-water distribution models, i.e., self-contained gas reservoir of structural-trap style in Songjiachang, anticline-fracture-cave composite trap pattern in Linantong and fracture-cave trap pattern in Hebaochang. In combination with geological background, it is thought that the hydrodynamic condition of different karst areas is the decisive factor of gas-water distribution, that the tectonic movement controls the regularity of the gas-water distribution, and that fluid potential indicates the activity of the water body.

       

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