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鄂西渝东区上二叠统吴家坪组页岩气地质条件及勘探潜力

梁西文 李乐

梁西文, 李乐. 鄂西渝东区上二叠统吴家坪组页岩气地质条件及勘探潜力[J]. 石油实验地质, 2021, 43(3): 386-394. doi: 10.11781/sysydz202103386
引用本文: 梁西文, 李乐. 鄂西渝东区上二叠统吴家坪组页岩气地质条件及勘探潜力[J]. 石油实验地质, 2021, 43(3): 386-394. doi: 10.11781/sysydz202103386
LIANG Xiwen, LI Le. Geological conditions and exploration potential for shale gas in Upper Permian Wujiaping Formation in the region of western Hubei-eastern Chongqing[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(3): 386-394. doi: 10.11781/sysydz202103386
Citation: LIANG Xiwen, LI Le. Geological conditions and exploration potential for shale gas in Upper Permian Wujiaping Formation in the region of western Hubei-eastern Chongqing[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(3): 386-394. doi: 10.11781/sysydz202103386

鄂西渝东区上二叠统吴家坪组页岩气地质条件及勘探潜力

doi: 10.11781/sysydz202103386
基金项目: 

国家科技重大专项“中扬子页岩气潜力分析与目标评价” 2017ZX05036-003-008

详细信息
    作者简介:

    梁西文(1966-), 男, 博士, 高级工程师, 从事油气勘探工作。E-mail: Liang_xw1966@126.com

    通讯作者:

    李乐(1985-), 男, 博士, 副研究员, 从事石油地质研究。E-mail: santali2005@gmail.com

  • 中图分类号: TE132.2

Geological conditions and exploration potential for shale gas in Upper Permian Wujiaping Formation in the region of western Hubei-eastern Chongqing

  • 摘要: 鄂西渝东区上二叠统吴家坪组页岩在早期勘探中已发现具备页岩气成藏条件,但其勘探潜力仍不明确。基于Jy3井岩心分析测试资料,结合区域地震、本井及周围井测井及录井等资料,对吴家坪组吴二段页岩的分布、页岩品质及含气性、保存条件及资源规模进行了分析。研究认为:吴二段发育深水陆棚及斜坡—浅水陆棚相富有机质泥页岩,具有南西薄、北东厚的区域分布规律。页岩主要由石英(平均含量43.10%)、黏土矿物(平均含量21.95%)及方解石(平均含量17.20%)所组成,有机质以Ⅱ1型干酪根为主,丰度高(总有机碳平均含量8.77%),热演化程度高(换算Ro平均为2.06%),孔隙性优良(孔隙度平均为5.59%),含气性好(总含气量平均为3.73 m3/t)。区内红星地区吴家坪组页岩厚度最大、保存条件良好,资源量最丰富,具有优越的页岩气勘探潜力及可观的资源前景,有望成为页岩气勘探开发接替层系及区块。

     

  • 图  1  鄂西渝东及其邻区主要构造单元划分

    据文献[36],有修改。

    Figure  1.  Tectonic units in western Hubei and eastern Chongqing and its adjacent areas

    图  2  鄂西渝东区上二叠统吴家坪组吴二段沉积相及页岩厚度等值线

    Figure  2.  Sedimentary facies and shale contour map of second member of Upper Permian Wujiaping Formation in western Hubei and eastern Chongqing

    图  3  鄂西渝东区上二叠统吴家坪组吴二段地层连井剖面对比

    对比路线见图 2

    Figure  3.  Cross well stratigraphic correlation section of second member of Upper Permian Wujiaping Formation in western Hubei and eastern Chongqing

    图  4  鄂西渝东区Jy3井上二叠统吴家坪组吴二段综合地质评价

    Figure  4.  Comprehensive geological evaluation of second member of Upper Permian Wujiaping Formation in well Jy3, western Hubei and eastern Chongqing

    图  5  鄂西渝东区上二叠统吴家坪组吴二段页岩中的有机质孔

    Figure  5.  Organic pores in second member of Upper Permian Wujiaping Formation in western Hubei and eastern Chongqing

    图  6  鄂西渝东区石柱复向斜龙驹坝构造(a)及建南构造(b)地震剖面

    剖面位置见图 1

    Figure  6.  Seismic profiles of Longjuba structure (a) and Jiannan structure (b) of Shizhu syncline in western Hubei and eastern Chongqing

    图  7  鄂西渝东区吴家坪组底界埋深

    Figure  7.  Burial depth of Wujiaping Formation in western Hubei and eastern Chongqing

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  • 收稿日期:  2020-07-13
  • 修回日期:  2021-03-15
  • 刊出日期:  2021-05-28

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