中国石油勘探 ›› 2018, Vol. 23 ›› Issue (4): 39-50.DOI: 10.3969/j.issn.1672-7703.2018.04.005

• 石油地质 • 上一篇    下一篇

湘鄂西地区下寒武统水井沱组页岩储层分布及非均质性特征

胡忠贵1,2, 秦鹏1,2, 胡明毅1,2, 邱小松3, 左洺滔1,2   

  1. 1 非常规油气湖北省协同创新中心;
    2 长江大学沉积盆地研究中心;
    3 中国石油勘探开发研究院
  • 收稿日期:2017-04-23 修回日期:2018-04-13 出版日期:2018-07-15 发布日期:2018-07-11
  • 基金资助:
    “十三五”国家科技重大专项“大型油气田及煤层气开发”(2016ZX05007002);湖北省教育厅科学技术研究计划重点项目“湘鄂西地区下寒武统牛蹄塘组页岩气储层非均质性及成因机理”(D20171302)。

The distribution and heterogeneity characteristics of shale reservoirs in Lower Cambrian Shuijingtuo Formation in western Hunan -Hubei region

Hu Zhonggui1,2, Qin Peng1,2, Hu Mingyi1,2, Qiu Xiaosong3, ZuoMingtao1,2   

  1. 1 Hubei Cooperative Innovation Center of Unconventional Oil and Gas;
    2 Research Center of Sedimentary Basin, Yangtze University;
    3 PetroChina Research Institute of Petroleum Exploration & Development
  • Received:2017-04-23 Revised:2018-04-13 Online:2018-07-15 Published:2018-07-11
  • Supported by:
     

摘要: 湘鄂西地区下寒武统水井沱组页岩储层研究程度相对较低,而页岩储层分布的不均一性严重制约了页岩气的勘探。以湘鄂西地区水井沱组页岩为研究对象,结合剖面和钻井资料,通过薄片、矿物含量、有机地球化学、扫描电镜等分析资料,分析了湘鄂西地区水井沱组页岩储层分布和非均质性特征。研究区有利页岩储层发育的相带为深水陆棚,以碳质页岩和硅质页岩为主。水井沱组划分为两个三级层序,Sq1时期以硅质陆棚为主,Sq2时期碳质陆棚分布更广。宏观上海侵体系域主要发育硅质页岩、碳质页岩,为富有机质页岩发育段;高位体系域主要发育钙质泥页岩、粉砂质泥页岩。微观上海侵体系域中页岩储层具有黏土矿物和有机碳含量向上逐渐升高,脆性矿物含量降低的特征,储集空间由基质孔向溶蚀孔、有机质孔演变,总孔隙度向上逐渐变大;高位体系域中页岩储层变化规律则相反。页岩储层分布的非均质性特征可能受到沉积时期海平面升降变化、物源供给以及生物作用的控制,也受到成岩作用、构造作用和水文地质作用的影响。

 

关键词: 湘鄂西地区, 水井沱组, 页岩储层, 非均质性

Abstract: The study on the shale reservoirs in the Lower Cambrian Shuijingtuo Formation in western Hunan-Hubei region are relatively less, and their heterogeneity severely limits the exploration of the shale gas. Taking the Shuijingtuo Formation shale as a target, and through analysis of thin sections, mineral content, organic geochemistry and SEM on profile and drilling data, the distribution and heterogeneity characteristics of the shale reservoirs in the Shuijingtuo Formation were studied. The result shows that the favorable facies for the development of the shale reservoirs is the deep water shelf, while dominated by carbonaceous shale and siliceous shale in the study area. The Shuijingtuo Formation is divided into two third-order sequences:the Sq1 is dominated by siliceous continental shelves, and the Sq2 is carbonaceous continental shelves more widely distributed. Macroscopically, siliceous and carbonaceous shales are developed in the transgressive system tract, which constitute an organic-rich shale zone; while calcareous and silty mud shales are developed in the highstand system tract. Microscopically, the shale reservoirs in the transgressive system tract have the features of increasing clay minerals and organic carbon content and decreasing brittle mineral content, and the reservoir space evolved from matrix pores to dissolved and organic pores, showing increasing total porosity; the shale reservoirs in the highstand system tract change in the opposite. The heterogeneous distribution of the shale reservoirs may be controlled by changes in sea level, source supply and biological effects, as well as diagenetic, tectonic and hydrogeological effects during the sedimentation.

Key words: western Hunan-Hubei region, Shuijingtuo Formation, shale reservoir, heterogeneity

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