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    北部湾盆地福山凹陷古近系双层结构形成机制

    林正良 王华 李红敬 马庆林 李媛 赵淑娥

    林正良, 王华, 李红敬, 马庆林, 李媛, 赵淑娥, 2015. 北部湾盆地福山凹陷古近系双层结构形成机制. 地球科学, 40(1): 169-178. doi: 10.3799/dqkx.2015.012
    引用本文: 林正良, 王华, 李红敬, 马庆林, 李媛, 赵淑娥, 2015. 北部湾盆地福山凹陷古近系双层结构形成机制. 地球科学, 40(1): 169-178. doi: 10.3799/dqkx.2015.012
    Lin Zhengliang, Wang Hua, Li Hongjing, Ma Qinglin, Li Yuan, Zhao Shu'e, 2015. Genetic Mechanism of Double-Layer Structure in Paleogene of Fushan Sag, Beibu Gulf Basin. Earth Science, 40(1): 169-178. doi: 10.3799/dqkx.2015.012
    Citation: Lin Zhengliang, Wang Hua, Li Hongjing, Ma Qinglin, Li Yuan, Zhao Shu'e, 2015. Genetic Mechanism of Double-Layer Structure in Paleogene of Fushan Sag, Beibu Gulf Basin. Earth Science, 40(1): 169-178. doi: 10.3799/dqkx.2015.012

    北部湾盆地福山凹陷古近系双层结构形成机制

    doi: 10.3799/dqkx.2015.012
    基金项目: 

    国家重点基础研究发展计划"973"项目 2014CB239201

    国家自然科学基金项目 41272722

    国家自然科学基金项目 41172123

    详细信息
      作者简介:

      林正良(1978-), 男, 博士, 高级工程师, 主要从事构造地质学方面的研究工作.E-mail: lzl-lll@163.com

    • 中图分类号: P618

    Genetic Mechanism of Double-Layer Structure in Paleogene of Fushan Sag, Beibu Gulf Basin

    • 摘要: 以北部湾盆地区域构造分析为基础, 在福山凹陷构造活动性研究的基础上探讨了福山凹陷形成的动力学机制, 分析了凹陷东部地区古近系地层中双层结构的形成机制问题.研究认为: 福山凹陷在平面上受红河断裂的左行走滑和海南隆起顺时针旋转的双重作用, 流三段沉积期凹陷在旋转-拉分作用下发生强烈的水平伸展, 为东部地区下构造层中的反向断层提供动力源, 海南隆起的快速隆升作用形成了上构造层中的重力滑动生长断层, 渐新统早期在流二段泥岩中发育的火成岩侵入体在凹陷的东部地区形成一道天然屏障, 最终形成双层结构.结果表明, 双层结构形成过程可划分为裂陷雏形期、下构造层伸展断裂期、中部塑性层发育期、上构造层形成期以及双层结构定形期5个主要阶段.

       

    • 图  1  福山凹陷构造位置

      Fig.  1.  The structural location map of Fushan sag

      图  2  双层结构典型地震剖面(剖面位置见图 1)

      Fig.  2.  Typical seismic section of double-layer structure

      图  3  福山凹陷地层与构造运动事件

      Fig.  3.  Strata and tectonic movement events of Fushan sag

      图  4  福山凹陷古近系主控断层走向演化及沉积中心演化

      A.长流组,1 000 m厚度等值线;B.流三段段,1 000m厚度等值线;C.流二段,500 m厚度等值线;D.流一段,1 000 m厚度等值线;E.涠三段+涠二段,800 m厚度等值线;F.涠一段,800 m厚度等值线

      Fig.  4.  The evolution of the main fault structure and deposition center of Fushan sag in Paleogene

      图  5  福山凹陷流二段侵入岩厚度分布

      Fig.  5.  The isopach map of the Intrusive rocks in the second member of the Liushagang Formation, Fushan sag

      图  6  福山凹陷南部斜坡带地层分布特征

      a.地层分布范围;b.地层产状

      Fig.  6.  Stratigraphic distribution characteristics of the south slope belt

      图  7  福山凹陷双层结构形成过程

      Fig.  7.  Schematic diagram for the formation process of double-layer structure of Fushan sag

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