中国石油勘探 ›› 2020, Vol. 25 ›› Issue (5): 32-42.DOI: 10.3969/j.issn.1672-7703.2020.05.005

• 勘探案例 • 上一篇    下一篇

川东北地区大安寨段陆相页岩气藏地质特征

周德华1,孙川翔2,刘忠宝2,聂海宽2   

  1. 1 中国石化油田勘探开发事业部;2 中国石化石油勘探开发研究院
  • 出版日期:2020-09-14 发布日期:2020-09-12
  • 基金资助:
    国家自然科学基金项目“四川盆地五峰组—龙马溪组页岩气储层演化机理及评价方法”(41872124);国家科技重大专项 项目“陆相层系页岩气勘探潜力评价”(2017ZX05036-004);中国石油化工股份有限公司科技开发部项目“川东北地区自流井组页岩气 富集主控因素与有利目标”(P19017)。

Geological characteristics of continental shale gas reservoir in the Jurassic Da’anzhai member in the northeastern Sichuan Basin

Zhou Dehua1,Sun Chuanxiang2, Liu Zhongbao2, Nie Haikuan2   

  1. 1 Department of Oilfi eld Exploration & Development, Sinopec; 2 Sinopec Petroleum Exploration and Production Research Institute
  • Online:2020-09-14 Published:2020-09-12
  • Supported by:
     

摘要: 为探索陆相页岩气藏地质特征及勘探开发潜力,以川东北元坝、涪陵地区侏罗系自流井组大安寨段为例, 通过岩心观察、薄片鉴定、X射线衍射、有机碳含量分析、扫描电镜、高压压汞和氮气吸附等测试手段,重点研究了 陆相页岩沉积环境与岩性、有机地球化学特征、储集空间与含气性、矿物组成、流体性质等气藏地质特征。研究结果 表明,大安寨段发育浅湖—半深湖相富有机质页岩,岩性以页岩夹条带状或薄层状砂岩、介壳灰岩为主,有机质类型 为Ⅱ2 型或Ⅲ型,TOC为0.33%~3.78%,R o 为 1.11%~1.82%,总体处于成熟—高成熟演化阶段;页岩储层以无机 质孔为主,孔隙度为1.5%~6.7%,以小于2nm的微孔和2~50nm的介孔为主,具有良好的含气性(含气量平均为 1.49m3/t);页岩可压裂性较好,脆性矿物含量平均达51%。已有12口井获高产油气流,总体表现出良好的勘探开 发潜力。在对比研究陆相页岩与海相页岩特征差异性基础上,进一步明确有利沉积相是川东北地区大安寨段陆相页岩 气富集高产的重要基础,同时受控于岩石组合及岩性成分、有机碳含量、物性参数、流体压力和微裂缝发育程度,以 上认识可为四川盆地侏罗系陆相页岩气最佳勘探开发层系优选提供依据。

 

关键词: 侏罗系, 大安寨段, 陆相页岩气, 四川盆地

Abstract: In this paper, continental shale gas reservoirs in the Da’anzhai member of the Jurassic Ziliujing Formation in the Yuanba and Fuling areas in the northeastern Sichuan Basin is studied to investigate the geological characteristics and exploration and development potential. Core analysis and lab test were conducted, including core observation, thin section identification, X-ray diffraction, organic carbon content analysis, Scanning Electron Microscope, high-pressure mercury injection and nitrogen adsorption, to determine the sedimentary environment and lithology, organic geochemical characteristics, reservoir space and gas-bearing properties, mineral composition and fluid properties of continental shale gas reservoir. The results show that organic- rich shales are developed in shallow to semi-deep lacustrine facies in the Da’anzhai member. The lithology is mainly shale intercalated with stripped or laminated sandstones and shell limestones. The organic matter type is Type Ⅱ2 or type Ⅲ. TOC is 0.33%?3.78%. Ro is 1.11%?1.82%, indicating a mature to high mature stage. The reservoir space in the shale is mainly mineral pores. The porosity ranges from 1.5% to 6.7%, with micro-pores less than 2nm and medium pores of 2?50 nm being the most prevalent. The gas-bearing properties are good (average gas content is 1.49 m3/t). The shale has good fracability and the average content of brittle minerals is 51%. A total of 12 wells have obtained high-production oil and gas flows, showing good exploration and development potential. Comparative study of the differences between the characteristics of continental shale and marine shale indicates that favorable sedimentary facies is an important basis in enrichment and high production of continental shale gas in the Da’anzhai member. Shale gas accumulation is also controlled by rock association and lithologic composition, organic carbon content, physical properties, fluid pressure, and the development degree of micro fractures. These understandings provide reference for selection of the most favorable exploration and development target formations of Jurassic continental shale gas in the Sichuan Basin.

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