天然气地球科学

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鄂尔多斯盆地东北缘叠置含气系统中菱铁质泥岩测井识别及地质意义

肖骞1,2,沈玉林1,2,秦勇1,2,申建1,2,顾娇杨3,张春良1,2   

  1. 1.中国矿业大学煤层气资源与成藏过程教育部重点实验室,江苏 徐州 221008;
    2.中国矿业大学资源与地球科学学院,江苏 徐州 221008;
    3.中联煤层气有限责任公司,北京 100011
  • 收稿日期:2016-12-02 修回日期:2017-01-18 出版日期:2017-04-10 发布日期:2017-04-10
  • 通讯作者: 沈玉林(1981-),男,安徽宣城人,副教授,博士,主要从事非常规天然气地质学与沉积学研究. E-mail:yulinsh@163.com.
  • 作者简介:肖骞(1991-),男,陕西西乡人,硕士研究生,主要从事沉积学研究. E-mail:cumtxq91@163.com.
  • 基金资助:

    国家自然科学基金项目(编号:41102100;41541046;41672146);国家科技重大专项项目(编号:2016ZX05044-002-001;2016ZX05066-001-004)联合资助.

The logging identification and the geological significance of the mudstone containing siderite in  multiple superposed coalbed-methane system in northeastern area of the Ordos Basin,China

Xiao Qian1,2,Shen Yu-lin1,2,Qin Yong1,2,Shen Jian1,2,Gu Jiao-yang3,Zhang Chun-liang1,2   

  1. 1.Key Laboratory of CBM Resources and Reservoir Formation Process,Ministry of Education,China University of Mining and Technology,Xuzhou 221008,China;
    2.School of Resources and Geoscience ,China University of Mining and Technology,Xuzhou 221008,China;3.China United Coalbed Methane Corporation Limited,Beijing  100011,China
  • Received:2016-12-02 Revised:2017-01-18 Online:2017-04-10 Published:2017-04-10

摘要:

以鄂尔多斯盆地东北缘地区本溪组_山西组菱铁质泥岩为研究对象,对研究区钻孔岩心与测井资料采用逻辑判别、蛛网图等方法,量化了研究区菱铁质泥岩的测井识别特征,建立其测井识别模板。研究表明,菱铁质泥岩具有高光电吸收截面指数(PE)、高密度(DEN)、高自然伽马(GR)、低声波时差(AC)、低电阻率(M2RX)、低中子孔隙度(CNCF)的特征,研究区12口钻孔中的菱铁质泥岩识别结果表明,总厚度为3.9~25.4m,总层数为8~28层,区域分布不均;通过测井资料定量分析了菱铁质泥岩的物性及封盖性能,指出研究区菱铁质泥岩具低孔低渗性及高突破压力的特点,其平均渗透率为2.29×10-8μm2、平均有效孔隙度为1.20%、平均突破压力为12.32MPa,在叠置含气系统中具备隔水阻气性能。基于菱铁质泥岩的空间发育位置,沉积环境及形成过程分析,在本溪组_山西组共识别出4个稳定隔水阻气层,结合气测资料将研究区本溪组_山西组垂向划分出5个独立含气系统,每个独立含气系统的边界便是区域分布稳定、连续性好且垂向发育具有一定规模的以菱铁质泥岩为主要岩层的隔层。

关键词: 菱铁质泥岩, 含气系统, 测井识别, 隔水阻气层, 鄂尔多斯盆地

Abstract:

This research quantifies the logging identification characteristics of the mudstone containing siderite and establishes its identification template accordingly using the method of logical analysis and the spider diagram analysis,based on the drill core observation and the logging data from Benxi Formation to Taiyuan Formation in the northeast area of the Ordos Basin.It is analyzed that the mudstone containing siderite has the features of high Photoelectric Absorption Coefficient(PE),high Density(DEN),high Natural Gamma(GR),low Interval Transit Time(AC),low Resistivity(M2RX) and low Neutron Porosity(CNCF).The results of siderite identification of 12 drills in the research area show that the mudstone containing siderite is unevenly distributed with the total thickness of 3.9-25.4m and the total layers of 8-28.It is concluded that mudstone containing siderite has the characteristics of low porosity,low permeability and high breakthrough pressure according to the quantitative analysis of the logging data.The average permeability,average effective porosity,and average breakthrough pressure of the mudstone containing siderite is 2.29×10-8μm2,1.20%,and 12.32MPa,respectively,which specifies its function as the impermeable gas barrier.Based on the spatial development position,sedimentary environment and forming process of the siderite containing siderite,four stable gas barriers are identified from Benxi Formation to Taiyuan Formation in the research area.The strata from Benxi Formation to Taiyuan Formation are divided into 5 independent Coalbed-Methane Systems combining the gas survey data.The boundary of each independent Coalbed-Methane System is the interlayer which develops a certain scale of rock stratum mainly consisting of mudstone containing siderite vertically and has the characteristics of stable area distribution and good continuity.

Key words: Mudstone containing siderite, Coalbed-Methane system, Logging identification, Impermeable gas barrier, Ordos Basin

中图分类号: 

  • TE132.1

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