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    陆相断陷湖盆迁移型层序构型及意义:以珠Ⅰ坳陷古近系文昌组为例

    朱红涛 李森 刘浩冉 舒誉 梅廉夫 杨香华

    朱红涛, 李森, 刘浩冉, 舒誉, 梅廉夫, 杨香华, 2016. 陆相断陷湖盆迁移型层序构型及意义:以珠Ⅰ坳陷古近系文昌组为例. 地球科学, 41(3): 361-372. doi: 10.3799/dqkx.2016.028
    引用本文: 朱红涛, 李森, 刘浩冉, 舒誉, 梅廉夫, 杨香华, 2016. 陆相断陷湖盆迁移型层序构型及意义:以珠Ⅰ坳陷古近系文昌组为例. 地球科学, 41(3): 361-372. doi: 10.3799/dqkx.2016.028
    Zhu Hongtao, Li Sen, Liu Haoran, Shu Yu, Mei Lianfu, Yang Xianghua, 2016. The Types and Implication of Migrated Sequence Stratigraphic Architecture in Continental Lacustrine Rift Basin: An Example from the Paleogene Wenchang Formation of Zhu Ⅰ Depression, Pearl River Mouth Basin. Earth Science, 41(3): 361-372. doi: 10.3799/dqkx.2016.028
    Citation: Zhu Hongtao, Li Sen, Liu Haoran, Shu Yu, Mei Lianfu, Yang Xianghua, 2016. The Types and Implication of Migrated Sequence Stratigraphic Architecture in Continental Lacustrine Rift Basin: An Example from the Paleogene Wenchang Formation of Zhu Ⅰ Depression, Pearl River Mouth Basin. Earth Science, 41(3): 361-372. doi: 10.3799/dqkx.2016.028

    陆相断陷湖盆迁移型层序构型及意义:以珠Ⅰ坳陷古近系文昌组为例

    doi: 10.3799/dqkx.2016.028
    基金项目: 

    国家科技重大专项课题 2011ZX05023-001-015

    国家自然科学基金项目 41572084

    详细信息
      作者简介:

      朱红涛(1976-),男,教授,博士生导师,主要从事层序地层学、地震沉积学与地震资料综合解释的教学与科研工作.E-mail: htzhu@cug.edu.cn

    • 中图分类号: P618.130

    The Types and Implication of Migrated Sequence Stratigraphic Architecture in Continental Lacustrine Rift Basin: An Example from the Paleogene Wenchang Formation of Zhu Ⅰ Depression, Pearl River Mouth Basin

    • 摘要: 相对于海相盆地层序,陆相盆地层序构型具有多样性特征.迁移型层序是陆相断陷湖盆演化过程中一种特殊的层序构型,研究相对较少.通过珠江口盆地珠Ⅰ坳陷惠州凹陷、恩平凹陷古近系文昌组层序迁移现象的分析,定义了迁移型层序的概念,划分出“自迁移”和“异迁移”两种迁移型层序类型.自迁移型层序是由低角度正断层的水平滑动造成,即由同一条同沉积边界断裂控制;异迁移型层序由盆地两侧同沉积控边断裂活动强度及先后期次造成,即由两条同沉积边界断裂控制.迁移型层序在侧向迁移过程中,不同级次的层序地层单元控制下的储层、烃源岩也发生侧向迁移、斜列叠置,更利于生、储、盖等油气成藏要素的有效配置,形成多区块、多层段油气藏组合.

       

    • 图  1  珠江口盆地珠Ⅰ坳陷文昌组洼陷划分及构造特征

      Fig.  1.  Sag units and tectonics of Paleogene Wenchang Formation of Zhu Ⅰ depression, Pearl River Mouth basin

      图  2  珠江口盆地珠Ⅰ坳陷古近系文昌组层序地层格架

      Fig.  2.  Sequence stratigraphic framework of Paleogene Wenchang Formation of Zhu Ⅰ depression, Pearl River Mouth basin

      图  3  珠Ⅰ坳陷恩平凹陷EP17洼文昌组自迁移层序构型

      剖面位置见图 1

      Fig.  3.  Typical autogenic migration sequence stratigraphic architecture across EP17 sub-sag of Enping sag, Zhu Ⅰ depression

      图  4  恩平凹陷EP17、EP12洼文昌组SQ1~SQ7层序北部沉积边界叠合

      Fig.  4.  Northern sedimentary boundary overlay distributions of Wenchang sequences SQ1-SQ7 of EP17 and EP12 sub-sags, Enping sag

      图  5  恩平凹陷文昌组SQ1~SQ7层序地层恢复剖面

      Fig.  5.  Balance section restoration of Wenchang sequences SQ1-SQ7 of Enping sag

      图  6  珠Ⅰ坳陷惠州凹陷HZ26-XJ24洼文昌组异迁移层序构型

      剖面位置见图 1

      Fig.  6.  Typical allogenic migration sequence stratigraphic architecture across HZ26 and XJ24 sub-sags of Huizhou sag, Zhu Ⅰ depression

      图  7  惠州凹陷HZ26洼、XJ24洼文昌组及三级层序SQ1~SQ7厚度平面分布

      Fig.  7.  Sequence stratigraphic thickness distributions of Wenchang Formation and third-order sequences SQ1-SQ7 of HZ26 and XJ24 sub-sags, Huizhou sag

      图  8  惠州凹陷HZ26洼、XJ24洼文昌组SQ1~SQ7层序地层恢复剖面

      Fig.  8.  Balance section restoration of Wenchang sequences SQ1-SQ7 of HZ26 and XJ24 sub-sags, Huizhou sag

      图  9  典型断陷湖盆层序(a)与迁移型层序(b.自迁移;c.异迁移)及其生-储组合

      Fig.  9.  Sequence stratigraphic architecture of classical rift basin (a) and migrated sequence stratigraphic architecture (b.autogenic migration, c.allogenic migration) and their reservoir-source rock couples

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