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鄂西海槽下寒武统水井沱组沉积特征及其油气地质意义

陈科 王昱荦 卢妍欣 李飞

陈科,王昱荦,卢妍欣,等,2025. 鄂西海槽下寒武统水井沱组沉积特征及其油气地质意义[J]. 地质力学学报,31(4):604−616 doi: 10.12090/j.issn.1006-6616.2025036
引用本文: 陈科,王昱荦,卢妍欣,等,2025. 鄂西海槽下寒武统水井沱组沉积特征及其油气地质意义[J]. 地质力学学报,31(4):604−616 doi: 10.12090/j.issn.1006-6616.2025036
CHEN K,WANG Y L,LU Y X,et al.,2025. Sedimentary characteristics of the Lower Cambrian Shuijingtuo Formation in the E’Xi trough and its petroleum geological significance[J]. Journal of Geomechanics,31(4):604−616 doi: 10.12090/j.issn.1006-6616.2025036
Citation: CHEN K,WANG Y L,LU Y X,et al.,2025. Sedimentary characteristics of the Lower Cambrian Shuijingtuo Formation in the E’Xi trough and its petroleum geological significance[J]. Journal of Geomechanics,31(4):604−616 doi: 10.12090/j.issn.1006-6616.2025036

鄂西海槽下寒武统水井沱组沉积特征及其油气地质意义

doi: 10.12090/j.issn.1006-6616.2025036
基金项目: 国家自然科学基金项目(U2344213)
详细信息
    作者简介:

    陈科(1982—),男,博士,正高级工程师,主要从事油气地质调查。Email:39024332@qq.com

    通讯作者:

    王昱荦(1997—),男,硕士,助理工程师,主要从事油气地质调查。Email:1197434674@qq.com

  • 中图分类号: P618.13

Sedimentary characteristics of the Lower Cambrian Shuijingtuo Formation in the E’Xi trough and its petroleum geological significance

Funds: This research is financially supported by the National Natural Science Foundation of China (Grant No. U2344213).
  • 摘要: 中国南方下寒武统富有机质页岩具有整体厚度大、热演化程度高的特点,近期的页岩气勘探已经在中扬子地区获得下寒武统页岩气工业气流。为了进一步调查中国南方下寒武统页岩气资源潜力,以中扬子地区下寒武统水井沱组为重点,结合地表露头观察和钻井资料,研究分析了其沉积特征和沉积过程,划分了下寒武统页岩三级地层层序格架,构建了中扬子地区鄂西海槽早寒武世的沉积模式,并指明了中扬子地区下寒武统页岩气勘探方向。研究表明:中扬子地区下寒武统水井沱组主要发育浅水陆棚相和深水陆棚相沉积,其底部和顶部发育浅水碳酸盐岩沉积;下寒武统富有机质页岩可划分为5个三级层序,并可与上扬子地区进行对比;水井沱组发育于震旦纪—早寒武世鄂西海槽的充填阶段,主要为泥质碎屑岩沉积。富有机质页岩分布于深水相区,在鄂西海槽识别出恩施、宜昌长阳2个次级凹陷,是页岩气勘探的重点地区;下寒武统水井沱组与下伏震旦系灯影组和陡山沱组形成“三明治”式常规油气组合,是下一步鄂西常规油气勘查的重点领域。

     

  • 图  1  扬子地区早寒武世古地理图(据Wang et al.,2012刘忠宝等,2018赵建华等,2019修改)

    Figure  1.  Paleogeographic map of the Yangtze region during the Early Cambrian(modified after Wang et al.,2012Liu et al.,2018Zhao et al.,2019

    图  2  典型野外剖面露头岩石特征

    a—宜昌鹤峰水井沱组与灯影组间平行不整合;b—宜昌滚石坳剖面水井沱组富有机质泥岩;c—宜昌滚石坳剖面水井沱组上部中—厚层灰岩夹薄层泥页岩;d—宜昌秭归泗溪剖面石牌组厚层灰黄色泥岩夹粉砂岩

    Figure  2.  Rock characteristics of typical outcrop sections

    (a) Disconformity between the Shuijingtuo Formation and the Dengying Formation at the Hefeng section in Yichang; (b) Organic-rich mudstone of the Shuijingtuo Formation at the Gunshi'ao section in Yichang; (c) Upper part of the Shuijingtuo Formation at the Gunshi'ao section in Yichang, characterized by medium-to-thick-bedded limestone interbedded with thin layers of mudstone and shale; (d) Thick-bedded grayish–yellow mudstone intercalated with siltstone of the Shipai Formation at the Sixi section in Zigui, Yichang

    图  3  鄂西海槽水井沱组典型沉积岩相

    Figure  3.  Typical sedimentary facies of the Shuijingtuo Formation in the E’Xi Trough

    图  4  中扬子地区下寒武统层序地层划分柱状图(剖面位置见图1;据王传尚等,2012修改

    Figure  4.  Sequence stratigraphic column of the Lower Cambrian in the Middle Yangtze Region (The location is shown in Fig.1; modified after Wang et al.,2012

    图  5  EYY1井综合柱状图

    Figure  5.  Comprehensive histogram of Well EYY1

    图  6  鄂西海槽地区水井沱组和岩家河组沉积厚度等值线图

    Figure  6.  Isopach map of the Shuijingtuo and Yanjiahe Formations in the E’Xi Trough area

    图  7  中扬子地区下寒武统近东—西方向连井剖面(剖面位置见图6)

    Figure  7.  E–W trending well-tie cross-section of the Lower Cambrian in the Middle Yangtze region (The location is shown in Fig.6.)

    图  8  中扬子地区下寒武统近北西—南东方向连井剖面(剖面位置见图6)

    Figure  8.  NW–SE trending well-tie cross-section of the Lower Cambrian in the Middle Yangtze region (The location is shown in Fig.6.)

    图  9  中上扬子地区下寒武统富有机质页岩沉积模式图(上扬子地区数据据刘忠宝等,2018修改

    Figure  9.  Depositional model of Lower Cambrian organic-rich shales in the Middle–Upper Yangtze region (The data for the Upper Yangtze region are modified from Liu et al.,2018

    表  1  中上扬子地区下寒武统地层对比表

    Table  1.   Stratigraphic correlation of the Lower Cambrian in the Middle–Upper Yangtze region

    四川盆地黔北中扬子
    寒武系沧浪铺组沧浪铺组石牌组
    筇竹寺组上段牛蹄塘组三段水井沱组上段
    下段二段下段
    麦地坪组一段岩家河组/天柱山段
    震旦系灯影组灯影组灯影组
    下载: 导出CSV
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出版历程
  • 收稿日期:  2025-04-03
  • 修回日期:  2025-07-15
  • 录用日期:  2025-07-20
  • 预出版日期:  2025-07-29
  • 刊出日期:  2025-08-28

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