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宜昌黄陵隆起构造演化及其对中下扬子页岩气勘探的启示

王步清 肖粤新 徐秋晨

王步清, 肖粤新, 徐秋晨, 2022. 宜昌黄陵隆起构造演化及其对中下扬子页岩气勘探的启示. 地质力学学报, 28 (4): 561-572. DOI: 10.12090/j.issn.1006-6616.2021130
引用本文: 王步清, 肖粤新, 徐秋晨, 2022. 宜昌黄陵隆起构造演化及其对中下扬子页岩气勘探的启示. 地质力学学报, 28 (4): 561-572. DOI: 10.12090/j.issn.1006-6616.2021130
WANG Buqing, XIAO Yuexin, XU Qiuchen, 2022. Structural evolution of the Huangling uplift, South China: Implications for the shale gas exploration in the middle and lower Yangtze River area. Journal of Geomechanics, 28 (4): 561-572. DOI: 10.12090/j.issn.1006-6616.2021130
Citation: WANG Buqing, XIAO Yuexin, XU Qiuchen, 2022. Structural evolution of the Huangling uplift, South China: Implications for the shale gas exploration in the middle and lower Yangtze River area. Journal of Geomechanics, 28 (4): 561-572. DOI: 10.12090/j.issn.1006-6616.2021130

宜昌黄陵隆起构造演化及其对中下扬子页岩气勘探的启示

doi: 10.12090/j.issn.1006-6616.2021130
基金项目: 

国家自然科学基金 42002173

中国地质调查局地质调查项目 DD20201111

详细信息
    作者简介:

    王步清(1974—),男,博士,研究员,主要从事含油气盆地构造和矿产规划研究。E-mail:23177896@qq.com

  • 中图分类号: P618.13

Structural evolution of the Huangling uplift, South China: Implications for the shale gas exploration in the middle and lower Yangtze River area

Funds: 

the National Natural Science Foundation of China 42002173

the Geological Survey Project of the China Geological Survey DD20201111

  • 摘要: 2013年以来,在四川盆地周缘黄陵隆起南部斜坡带的下寒武统、震旦系取得页岩气勘查的重大发现和突破,开拓了盆外复杂构造区页岩气勘查新方向。依据已有研究成果、区域地质资料、物探资料和钻井资料等,提出黄陵隆起从元古界以来经历了前震旦纪结晶基底形成、震旦纪初的岩体侵入、震旦纪—中侏罗世沉降沉积与隆升剥蚀交替发展、晚侏罗世—古近纪快速隆升削顶4个构造演化阶段。黄陵隆起独特的构造演化史对页岩气成藏起到了重要作用,其中震旦纪—中侏罗世沉降沉积与隆升剥蚀交替发展使早期烃源岩埋深适当,热演化程度和孔隙度适中;而强硬基底则保护了沉积盖层的相对完整性和连续性。考虑构造演化史、基底特征、盖层发育以及烃源岩等因素,对中、下扬子地区类似古隆起进行系统梳理分析,发现四川盆地外围的雪峰隆起、黔中隆起与南华北盆地的霍邱隆起石油地质条件较好,通过进一步的地质地球物理和钻探工作,有望取得油气调查的发现和突破。

     

  • 图  1  黄陵隆起及周边地质简图(据程裕淇等,2004修改)

    Figure  1.  Geological sketch map of the Huangling uplift and its periphery(modified from Cheng et al., 2004)

    图  2  黄陵隆起大地构造位置图(据郭战峰等,2006修改)

    Figure  2.  Tectonic location map of the Huangling uplift(modified from Guo et al., 2006)

    图  3  黄陵隆起构造演化模式图

    Figure  3.  Structural evolution pattern graph of the Huangling uplift

    图  4  黄陵隆起南侧地震解释剖面(据陈科等,2020修改)

    Figure  4.  Seismic interpretation profile of the southern Huangling uplift(modified from Chen et al., 2020)

    图  5  黄陵隆起西翼构造剖面(据邓铭哲,2018修改)

    Figure  5.  Structural section of the western flank of the Huangling Uplift(modified from Deng, 2018)

    图  6  霍邱隆起及周缘构造单元划分图

    Figure  6.  Structural units of the Houqiu uplift and its periphery

    图  7  过霍邱古隆起南北向结构剖面及可能的气藏类型(平面位置见图 6)

    Figure  7.  NS-trending structural section over the Huoqiu uplift and possible gas reservoir types(see Fig. 6 for the planar position)

    表  1  中、下扬子地区部分古隆起地质特征

    Table  1.   Geological characteristics of paleo-uplifts in the middle-lower Yangtze River area

    古隆起名称 地理位置 形成时代 隆起性质 基底 主要盖层 烃源岩发育特征 数据来源
    烃源岩层 TOC/% RO/%
    黄陵 湖北宜昌 晚侏罗世 挤压隆升 晚太古代—早元古代变质岩和新元古代花岗岩 震旦系—白垩系 陡山沱组
    牛蹄塘组
    龙马溪组
    2.3
    5.35
    2.56
    2.5~3.0
    1.4~2.8
    1.9~2.3
    李浩涵等,2017翟刚毅等,2017a陈科等,2020
    乐山-龙女寺 四川乐山、内江 石炭纪末 剥蚀古隆起 前震旦系花岗岩 震旦系—第四系,缺泥盆系、石炭系 陡山沱组
    龙马溪组
    3.20
    1.65
    4.0
    2.55
    梅庆华,2015
    汉南 陕西汉中-四川巴中 志留纪末 克拉通边缘翘倾古隆起 元古界结晶基底 震旦系—侏罗系 牛蹄塘组 4.22 2.66 陈相霖等,2018
    雪峰 湘西、黔东、桂北 志留纪末 陆内抬升与挤压褶皱隆起 前震旦褶皱基底 震旦系—第三系 牛蹄塘组
    龙马溪组
    1~22
    1~4
    2.0~3.55
    2.0~2.5
    邓大飞等,2014彭中勤等,2019
    黔中 贵州翁安、修文 奥陶纪末 克拉通内构造隆起 中元古界褶皱基底 寒武系—三叠系 牛蹄塘组
    龙马溪组
    石炭—二叠系
    2~6
    1~4
    0.23~3.67
    3.5~4.5
    2.5~3.5
    1.75~2.2
    陈相霖等,2021翟刚毅等,2017b
    九岭 江西宜丰、奉新 奥陶纪末 板块内部挤压隆起 晋宁期花岗岩 南华系—寒武系 王音铺—观音堂组 3.4 3.2 李建青等,2018
    许村 皖南歙县 —— —— 花岗闪长岩 寒武系 荷塘组 2~8 1.9~3.5 李建青等,2018
    霍邱 安徽长峰、合肥 三叠纪末 剥蚀古隆起 太古界花岗岩 寒武系—二叠系、侏罗系 寒武系
    石炭—二叠系
    4~8
    3
    3~4
    1.2
    石砥石等,2019
    下载: 导出CSV
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  • 收稿日期:  2021-09-28
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