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    雪峰山前陆盆地下志留统页岩气勘探潜力

    刘辰生 郭建华 王宗秀

    刘辰生, 郭建华, 王宗秀, 2019. 雪峰山前陆盆地下志留统页岩气勘探潜力. 地球科学, 44(11): 3678-3691. doi: 10.3799/dqkx.2019.208
    引用本文: 刘辰生, 郭建华, 王宗秀, 2019. 雪峰山前陆盆地下志留统页岩气勘探潜力. 地球科学, 44(11): 3678-3691. doi: 10.3799/dqkx.2019.208
    Liu Chensheng, Guo Jianhua, Wang Zongxiu, 2019. Potential for Shale Gas Exploration of Xuefengshan Foreland Basin of Lower Silurian. Earth Science, 44(11): 3678-3691. doi: 10.3799/dqkx.2019.208
    Citation: Liu Chensheng, Guo Jianhua, Wang Zongxiu, 2019. Potential for Shale Gas Exploration of Xuefengshan Foreland Basin of Lower Silurian. Earth Science, 44(11): 3678-3691. doi: 10.3799/dqkx.2019.208

    雪峰山前陆盆地下志留统页岩气勘探潜力

    doi: 10.3799/dqkx.2019.208
    基金项目: 

    湖南省自然科学基金项目 2017JJ1034

    中国地质调查局油气调查项目 DD20160183

    详细信息
      作者简介:

      刘辰生(1976-), 男, 副教授, 博士, 从事沉积学、油气地质学研究及相关教学工作

    • 中图分类号: P618

    Potential for Shale Gas Exploration of Xuefengshan Foreland Basin of Lower Silurian

    • 摘要: 雪峰山志留系前陆盆地分布在湘中-湘西北-四川盆地,是上扬子板块主要的盆地类型,目前针对该前陆盆地沉积特征和页岩气勘探潜力的研究少见.根据野外资料、测井资料和分析测试资料分析了湘西北和湘中地区前陆盆地沉积建造过程和页岩气勘探潜力.结果表明湘中前陆盆地前渊带以浊积扇和浅海陆棚相沉积为主,而湘西北隆后盆地沉积相类型丰富,包括潮坪相、浅海陆棚相、滨岸相、三角洲相和碳酸盐岩台地相等.虽然前渊带和隆后盆地沉积相类型和沉积厚度差异较大,但沉积旋回的划分却是一致的,因此前渊带和隆后盆地相互连通,雪峰山对其两侧盆地的遮挡作用有限.地球化学测试分析表明研究区隆后盆地页岩的有机碳含量、有机质类型均较四川盆地的焦石坝差.湖南地区志留系页岩各项地化指标较差的主要原因是其缺少龙马溪组第一旋回的黑色碳质页岩.

       

    • 图  1  上扬子志留系前陆盆地示意及研究区位置

      Fig.  1.  Sketch figure of foreland basin in the Upper Yangtze and the study area

      图  2  湖南省志留纪地层分布及分区

      1.露头分布区;2.地层分区界限;3.剖面位置;4.湘北区;5.雪峰山地区;6.剥蚀区(无沉积记录);7.研究区位置;8.地名;9.图 1剖面位置

      Fig.  2.  Distribution zone of Silurian in Hunan Province

      图  3  湘西北龙山比洞志留系剖面

      Fig.  3.  Section of Silurian in Longshanbidong, Northwest Hunan

      图  4  湘西北龙马溪组沉积特征

      a.龙山比洞剖面龙马溪组浅海陆棚相页岩;b.长峰村剖面页岩中发育的笔石

      Fig.  4.  Sedimentary characteristics of Longmaxi Formation in Northwest Hunan

      图  5  湘西北永页2井下志留统沉积相划分

      秦明阳等(2018)

      Fig.  5.  Facies division of Well Yongye 2 of Lower Silurian in Northwest Hunan

      图  6  湘西北罗惹坪组沉积特征

      a.茅草坪潮坪相潮上带和潮下带沉积特征;b.永顺三角洲相砂岩与泥页岩;c.吴家院滨岸相石英砂岩;d.龙山比洞碳酸盐岩台地相生物灰岩

      Fig.  6.  Sedimentary characteristics of Luoreping Formation in Northwest Hunan

      图  7  湘中地区龙马溪组浊积岩沉积特征

      a.横溪浊积砂岩与暗色页岩互层;b.横溪具鲍马序列的杂砂岩;c.横溪罗惹坪组石英杂砂岩(单偏光);d.横溪浊积岩与泥岩侵蚀接触关系

      Fig.  7.  Turbidite characteristics deposited in Longmaxi Formation in Northwest Hunan

      图  8  湘西北-湘中龙山比洞-横溪志留系沉积相对比(雪峰山隆起纵向比例夸大)

      Fig.  8.  Facies correlation of Silurian of Bidong in Longshan-Wentang-Maocaopu in Taoyuan-Hengxi, northwest-central Hunan (vertical exaggeration)

      图  9  湖南地区龙马溪组沉积相平面图

      a.龙马溪组早期沉积相平面图;b.龙马溪组晚期沉积相平面图

      Fig.  9.  Facies plan maps of Longmaxi Formation in Hunan area

      图  10  湖南地区罗惹坪组沉积相平面图

      Fig.  10.  Facies plan map of Luoreping Formation in Hunan area

      图  11  湖南地区龙马溪组页岩样品X衍射矿物成分

      Fig.  11.  Mineral compositions of Longmaxi Formation samples from X- ray diffraction in Hunan area

      图  12  重庆石柱-湖南桑植淋溪河-湖南温塘志留系旋回对比

      Fig.  12.  Cycle correlation of Silurian of Shizhu in Chongqing-Linxihe in Sangzhi-Wentang in Hunan

      表  1  湘西北隆后盆地永页2井龙马溪组-罗惹坪组TOC及含气量

      Table  1.   TOC and gas content of Longmaxi and Luoreping Formations in Well Yongye 2, Longhou basin, Northwest Hunan

      深度(m) 岩性 笔石 TOC(%) 总含气量(m3·t-1) 解析气(m3·t-1) φ(CH4)(%)
      罗惹坪组 1 300~1 485 灰色页岩 未见 0.10~0.50 < 0.1 < 0.10 10~40
      龙马溪组 1 485~1 508 灰黑色页岩 一般 0.12~0.74 < 1 < 0.10 84~95
      龙马溪组 1 508~1 518 灰黑色粉砂质页岩 丰富 1.00~2.81 1.00~2.00 0.50~1.00 92~96
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    • 收稿日期:  2019-08-25
    • 刊出日期:  2019-11-15

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