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鄂西地区震旦系—寒武系页岩气成藏模式

翟刚毅 王玉芳 刘国恒 陆永潮 何生 周志 李娟 张云枭

翟刚毅, 王玉芳, 刘国恒, 等, 2020. 鄂西地区震旦系—寒武系页岩气成藏模式. 地质力学学报, 26 (5): 696-713. DOI: 10.12090/j.issn.1006-6616.2020.26.05.058
引用本文: 翟刚毅, 王玉芳, 刘国恒, 等, 2020. 鄂西地区震旦系—寒武系页岩气成藏模式. 地质力学学报, 26 (5): 696-713. DOI: 10.12090/j.issn.1006-6616.2020.26.05.058
ZHAI Gangyi, WANG Yufang, LIU Guoheng, et al., 2020. Accumulation model of the Sinian-Cambrian shale gas in western Hubei Province, China. Journal of Geomechanics, 26 (5): 696-713. DOI: 10.12090/j.issn.1006-6616.2020.26.05.058
Citation: ZHAI Gangyi, WANG Yufang, LIU Guoheng, et al., 2020. Accumulation model of the Sinian-Cambrian shale gas in western Hubei Province, China. Journal of Geomechanics, 26 (5): 696-713. DOI: 10.12090/j.issn.1006-6616.2020.26.05.058

鄂西地区震旦系—寒武系页岩气成藏模式

doi: 10.12090/j.issn.1006-6616.2020.26.05.058
基金项目: 

国家科技重大专项项目 2016ZX05034

中国地质调查局地质调查项目 DD20190108

详细信息
    作者简介:

    翟刚毅(1958-),男,教授级高级工程师,主要从事油气和页岩气基础地质调查及资源潜力评价等方面的研究。E-mail:zhaigangyi@126.com

    通讯作者:

    王玉芳(1977-),女,高级工程师,主要从事页岩气战略选区调查评价及页岩气压裂试气等方面的研究。E-mail:147444819@qq.comE-mail

  • 中图分类号: P618.13

Accumulation model of the Sinian-Cambrian shale gas in western Hubei Province, China

  • 摘要: 通过对鄂西震旦系陡山沱组和寒武系牛蹄塘组页岩气勘查大量实际资料总结研究,创新性地提出了针对鄂西地区震旦系和寒武系"岩相控炭、成岩控烃、构造控藏"的页岩气成藏理论认识。震旦系陡山沱组和寒武系牛蹄塘组富有机质页岩沉积受控于鄂西裂陷海槽,富有机质页岩甜点层段主要形成于海侵体系域和早期高水位体系域。黄陵古隆起周缘震旦纪—三叠纪长期浅埋,为生油提供了充足时间,三叠纪短暂快速深埋,为页岩气生成的主峰期。古隆起刚性基底、区域性泥页岩盖层以及后期逆冲推覆构造,为页岩气保存提供了良好的条件。从而建立了鄂西震旦—寒武系"深水海槽控炭、古隆起浅埋控烃、古隆起+逆冲断裂控藏"的页岩气成藏模式。

     

  • 图  1  黄陵背斜及周缘地区构造单元划分

    Figure  1.  Division of structural units in the Huangling anticline and its surrounding areas

    图  2  页岩岩相划分

    N—牛蹄塘组;D—陡山沱组

    Figure  2.  Division of shale lithofacies

    图  3  鄂阳页1井陡山沱组高频层序单元划分柱状图

    Figure  3.  Histogram of high frequency sequence unit division of the Doushantuo Formation in the Eyangye No.1 well

    图  4  鄂阳页1井牛蹄塘组高频层序单元划分柱状图

    Figure  4.  Histogram of high frequency sequence unit division of the Niutitang Formation in the Eyangye No.1 well

    图  5  鄂西地区牛蹄塘组富有机质泥页岩横向展布图

    Figure  5.  Lateral distribution of organic-rich shales in the Niutitang Formation, western Hubei

    图  6  牛蹄塘组页岩TOC含量与沉积体系域关系图

    Figure  6.  Relationship between TOC content and sedimentary system tract of the Niutitang Formation shale

    图  7  宜昌地区陡山沱组和牛蹄塘组页岩部分样品热声发射突变温度记录结果图

    Figure  7.  Acoustic emission maps of some samples from the Doushantuo and Niutitang Formations in Yichang area

    图  8  页岩干酪根红外光谱最小波数(Wmin)与镜质体反射率关系图

    Figure  8.  Relationship between minimum wavenumber (Wmin) of infrared spectrum and vitrinite reflectance of shale kerogen

    图  9  黄陵背斜及周缘地区下寒武统牛蹄塘组黑色页岩成熟度分布图

    Figure  9.  Distribution map of maturity of black shale in the Niutitang Formation of Lower Cambrian in the Huangling anticline and its surrounding areas

    图  10  鄂阳页1井陡山沱组页岩裂缝石英脉中气-液两相盐水包裹体均一温度分布直方图和相关关系图

    Figure  10.  Histogram and correlation diagram of homogenization temperature distribution of gas-liquid two-phase brine inclusions in fractured quartz veins of the Doushantuo Formation in the Eyangye No.1 well

    图  11  鄂阳页1井牛蹄塘组页岩裂缝方解石脉气-液两相盐水包裹体均一温度分布直方图

    Figure  11.  Histogram of homogenization temperature distribution of gas-liquid two-phase brine inclusions in shale fractured calcite vein of the Niutitang Formation in the Eyangye No.1 well

    图  12  黄陵隆起及周缘构造演化、地温和抬升史概略图

    Figure  12.  Outline of tectonic evolution, geotemperature and uplift history of the Huangling uplift and its surrounding areas

    图  13  秭地2井陡山沱组和牛蹄塘组页岩埋藏—热演化—抬升史模拟重建图

    Figure  13.  Reconstruction of shale burial-thermal evolution-uplift history of the Doushantuo and Niutitang Formations in the Zidi No.2 well

    图  14  秭地2井陡山沱组和牛蹄塘组页岩模拟镜质体反射率和生烃史演化模拟图

    Figure  14.  Simulated vitrinite reflectance and hydrocarbon generation evolution of the Doushantuo and Niutitang shales in the Zidi No.2 well

    图  15  天阳坪断裂下盘鄂阳页1井页岩气富集成藏模式图

    Figure  15.  Shale gas enrichment and accumulation pattern of the Eyangye No.1 well in the footwall of the Tianyangping fault

    表  1  鄂西地区陡山沱组和牛蹄塘组钻井实测TOC含量统计表

    Table  1.   Statistical table of measured TOC content in drilling of the Doushantuo Formation and Niutetang Formation in western Hubei Province

    井号 陡山沱组页岩TOC含量/% 牛蹄塘组页岩TOC含量/%
    鄂阳页1井 1.00~2.90/1.70(295) 4.42~6.65/5.34(16)
    鄂宜参1井 0.13~4.0/0.92(?) 0.52~5.96/2.26(32)
    秭地1 0.72~2.91/1.63(19) 0.53~8.72/2.95(40)
    秭地2 0.07~1.78/0.66(22) 0.30~9.59/2.34(44)
    注:表中1.00~2.90为TOC测试样品值范围;1.70为TOC平均值;(295)为测试样品数
    下载: 导出CSV

    表  2  鄂西地区震旦系陡山沱组与牛蹄塘组实测有机质成熟度统计表

    Table  2.   Statistics of measured organic matter maturity in the Doushantuo Formation and Niutitang Formation of Sinian system in western Hubei Province

    测试方法 陡山沱组Ro/% 牛蹄塘组Ro/%
    固体沥青反射率 3.09~3.49/3.21(9) 2.84~3.24/3.02(11)
    干酪根红外光谱 2.3~3.3 1.7~2.6
    干酪根激光拉曼 /2.84(13) /3.08
    注:表中3.09~3.49为测试样品值范围;3.21为平均值;(9)为测试样品数
    下载: 导出CSV

    表  3  鄂阳页1井陡山沱组和牛蹄塘组页岩裂缝脉体样品信息表

    Table  3.   Information table of shale fractured vein samples from the Doushantuo Formation and Jiutitang Formation in the Eyangye No.1 well

    样品编号 采样层位 深度/m 脉体类型 脉体产状
    N-2 牛蹄塘组( 1n) 2942.56 方解石脉 高角度
    N-4 3062.00
    D-5 陡山沱组(Z1ds) 3357.72 石英脉为主
    D-7 3363.64
    D-10 3371.68
    D-12 3374.84
    D-20 3381.45
    D-21 3392.42
    下载: 导出CSV
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  • 收稿日期:  2020-08-21
  • 修回日期:  2020-08-31
  • 刊出日期:  2020-10-30

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