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海陆过渡相优质页岩测井识别: 以鄂尔多斯盆地大宁-吉县地区山2段为例

史彪 吴丰 李树新 梁芸 习研平 代槿 石祥超 赵辉

史彪, 吴丰, 李树新, 梁芸, 习研平, 代槿, 石祥超, 赵辉. 海陆过渡相优质页岩测井识别: 以鄂尔多斯盆地大宁-吉县地区山2段为例[J]. 地质科技通报, 2023, 42(2): 115-126. doi: 10.19509/j.cnki.dzkq.2022.0107
引用本文: 史彪, 吴丰, 李树新, 梁芸, 习研平, 代槿, 石祥超, 赵辉. 海陆过渡相优质页岩测井识别: 以鄂尔多斯盆地大宁-吉县地区山2段为例[J]. 地质科技通报, 2023, 42(2): 115-126. doi: 10.19509/j.cnki.dzkq.2022.0107
Shi Biao, Wu Feng, Li Shuxin, Liang Yun, Xi Yanping, Dai Jin, Shi Xiangchao, Zhao Hui. Logging identification of high-quality shale of the marine-continent transitional facies: An example of the Shan 2 Member of the Daning-Jixian area in the Ordos Basin[J]. Bulletin of Geological Science and Technology, 2023, 42(2): 115-126. doi: 10.19509/j.cnki.dzkq.2022.0107
Citation: Shi Biao, Wu Feng, Li Shuxin, Liang Yun, Xi Yanping, Dai Jin, Shi Xiangchao, Zhao Hui. Logging identification of high-quality shale of the marine-continent transitional facies: An example of the Shan 2 Member of the Daning-Jixian area in the Ordos Basin[J]. Bulletin of Geological Science and Technology, 2023, 42(2): 115-126. doi: 10.19509/j.cnki.dzkq.2022.0107

海陆过渡相优质页岩测井识别: 以鄂尔多斯盆地大宁-吉县地区山2段为例

doi: 10.19509/j.cnki.dzkq.2022.0107
基金项目: 

中国石油-西南石油大学创新联合体科技合作项目 2020CX030103

四川省重点研发计划(重大科技专项)项目 2020YFSY0039

国家自然科学基金区域创新发展联合基金项目 U20A20266

详细信息
    作者简介:

    史彪(1998-), 男, 现正攻读地质资源与地质工程专业硕士学位, 主要从事测井原理及地质应用研究工作。E-mail: 1763515317@qq.com

    通讯作者:

    吴丰(1983-), 男, 副教授, 主要从事测井原理及地质应用方面的研究工作。E-mail: wufengzh@swpu.edu.cn

  • 中图分类号: P631.8

Logging identification of high-quality shale of the marine-continent transitional facies: An example of the Shan 2 Member of the Daning-Jixian area in the Ordos Basin

  • 摘要:

    鄂尔多斯盆地东南缘海陆过渡相地层矿物组成复杂,页岩与砂岩、煤等岩性频繁交互,岩性纵向变化快。由于常规测井曲线分辨率较低,且扩径现象普遍,导致海相页岩气评价中常用的岩性识别与优质页岩识别方法效果较差。首先利用反褶积技术提高自然伽马、无铀伽马和铀测井曲线分辨率,然后通过测井交会图组合图版分别识别海陆过渡相地层岩性和页岩岩相,进一步通过新提出的铀-自然电位曲线重叠法识别海陆过渡相优质页岩。结果表明:反褶积技术能有效提高自然伽马、无铀伽马和铀曲线分辨率,利用自然伽马-密度测井交会图识别海陆过渡相地层岩性效果较好;铀-无铀伽马交会图能进一步识别3种岩相页岩(钙质硅质页岩、硅质黏土质页岩和黏土质页岩);在海陆过渡相地层中,新提出的铀-自然电位重叠法比传统ΔlogR法识别优质页岩效果更好。本研究可为海陆过渡相页岩气储层测井评价提供理论支持,提高优质页岩识别准确率。

     

  • 图 1  大宁-吉县地区地理位置、地层划分及山23亚段海陆过渡相页岩厚度分布

    Figure 1.  Geographical location, stratigraphic division of the Daning-Jixian area and thickness distribution of shale in the transitional facies of the Shan23 submember

    图 2  大宁-吉县地区山2段海陆过渡相不同岩相页岩的岩心、薄片和扫描电镜照片

    a, d, g.钙质硅质页岩; b, e, h.硅质黏土质页岩; c, f, i.黏土质页岩;a.2 296.37 m,灰黑色钙质硅质页岩,岩心照片;b.2 123.20 m,灰黑色硅质黏土质页岩,砂质条带发育,岩心照片;c.2 023.60 m,灰黑色黏土质页岩,岩心照片;d.2 301.02 m,钙质硅质页岩,有机质发育,电镜照片;e.2 260.07 m,硅质黏土质页岩,砂质纹层,薄片照片;f.2 274.00 m,黏土质页岩,薄片照片;g.2 301.02 m,钙质硅质页岩中有机质孔大量发育,电镜照片;h.2 283.45 m,硅质黏土质页岩的有机质孔,电镜照片;i.2 278.32 m,黏土质页岩中黏土矿物层间裂隙,电镜照片

    Figure 2.  Core, thin section and scanning electron microscope photographs of different lithofacies shale in the marine-continent transitional facies of the Shan 2 Member in the Daning-Jixian area

    图 3  大宁-吉县地区山2段页岩岩相划分、黏土矿物类型及比例

    a.海陆过渡相页岩岩相划分三角图;b.3种不同岩相页岩黏土矿物成分及含量图

    Figure 3.  Lithofacies, and types and proportions of clay minerals of the shale in the Shan 2 Member of the Daning-Jixian area

    图 4  薄层的测井响应褶积原理示意

    Figure 4.  Schematic diagram of the convolution principle of the logging response of the thin layer

    图 5  反褶积法提高海陆过渡相地层GR曲线分辨率效果

    Figure 5.  Effect of the deconvolution method on improving the resolution of GR curves in the marine-continent transitional facies

    图 6  2段3种岩相页岩测井响应特征及镜下照片

    Figure 6.  Log response characteristics and micro photographs of three types of lithofacies shale in the Shan 2 Member

    图 7  2段海陆过渡相地层岩性与页岩岩相识别图版

    a.页岩识别图版;b.三种不同岩相页岩细分图版

    Figure 7.  Lithology and shale facies identification chart of the marine-continent transitional facies in the Shan 2 Member

    图 8  ΔlogR法和U-SP重叠法识别海陆过渡相优质页岩原理

    a.ΔlogR法识别优质页岩,效果较差;b.U-SP曲线重叠法识别优质页岩,效果好

    Figure 8.  Principles of the ΔlogR method and the U-SP overlap method to identify high-quality shale of the marine-continent transitional facies

    图 9  大吉51井山2段海陆过渡相优质页岩识别结果

    Figure 9.  Recognition results of high-quality shale from the marine-continent transitional facies of the Shan 2 Member, Well Daji51

    图 10  大宁-吉县地区山2段海陆过渡相优质页岩横向展布

    Figure 10.  Horizontal distribution of high-quality shale of the marine-continent transitional facies in the Shan 2 Member of the Daning-Jixian area

    表  1  不同沉积相优质页岩气储层关键参数对比

    Table  1.   Comparison of key parameters of high-quality shale gas reservoirs from different sedimentary facies

    沉积环境 学者 研究对象 优质页岩气储层关键参数
    脆性矿物体积分数/% 孔隙度/% w(TOC)/% 渗透率/10-3 μm2 含气量/(m3·t-1)
    海相 聂海宽等[33](2009) Barnett Shale, Fort Worth Basin / 5~6 2 <0.01 5.5
    贾成业等[34](2017) 四川盆地,昭通区块,龙马溪组页岩 69 / 3.2 / 4.8
    Wu Hengzhi[35](2019) 四川盆地,威远区块,五峰-龙马溪组页岩 60 6 5 / 5
    陆相 孙玉凯等[36](2010) 吐哈盆地,水西沟群和小沟群页岩 50 / 1 / 1
    姜呈馥等[37](2013) 鄂尔多斯盆地,延长组,长7段页岩 57 3.8 3.9 0.068 1.25~6.45
    王香增等[38](2014) 鄂尔多斯盆地,甘泉地区,延长组 50 2 2 <0.01 2~8
    海陆过渡相 闫德宇等[39](2013) 鄂尔多斯盆地,山西组和太原组页岩 50 4 2.1 0.037 /
    匡立春等[2](2020) 鄂尔多斯盆地,山西组页岩 50 2 2 / 2
    下载: 导出CSV
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