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    可容纳空间转换系统的定量模拟

    朱红涛 LiuKey u 杜远生 李敏 王继立

    朱红涛, LiuKey u, 杜远生, 李敏, 王继立, 2009. 可容纳空间转换系统的定量模拟. 地球科学, 34(5): 819-828.
    引用本文: 朱红涛, LiuKey u, 杜远生, 李敏, 王继立, 2009. 可容纳空间转换系统的定量模拟. 地球科学, 34(5): 819-828.
    ZHU Hong-tao, Liu Key u, DU Yuan-sheng, LI Min, WANG Ji-li, 2009. Quantitative Simulation and New Consideration on the Transformation System of the Accommodation Space. Earth Science, 34(5): 819-828.
    Citation: ZHU Hong-tao, Liu Key u, DU Yuan-sheng, LI Min, WANG Ji-li, 2009. Quantitative Simulation and New Consideration on the Transformation System of the Accommodation Space. Earth Science, 34(5): 819-828.

    可容纳空间转换系统的定量模拟

    基金项目: 

    国家自然科学基金 40702024

    详细信息
      作者简介:

      朱红涛(1976-), 男, 副教授, 博士后, 研究方向为层序地层学.E-mail: zhuht-oscar@yahoo.com.cn

    • 中图分类号: P539.2

    Quantitative Simulation and New Consideration on the Transformation System of the Accommodation Space

    • 摘要: 为探讨盆地两侧可容纳空间和层序叠加模式的非一致性变化, 利用SEDPAK二维层序模拟软件, 通过考虑控制层序沉积过程的不同参数, 对可容纳空间转换系统进行定量模拟并提出新的认识.模拟结果表明, 盆地两侧同期层序叠加模式可以分为"同步"和"非同步"两种, 同步叠加模式多出现在层序的低位体系域及高位体系域后期, 非同步叠加模式多出现在层序的水进体系域及高位体系域初期.多种地质参数的合理组合, 盆地两侧同期层序均可形成非同步叠加模式.非同步叠加模式对体系域界面的识别、层序对比具有一定的参考价值.

       

    • 图  1  构造活动以支点做“跷跷板”式运动(可容纳空间转换系统, 据Jiang et al., 2005修改)

      A.支点左侧沉降, 右侧抬升; B.支点左侧抬升, 右侧沉降

      Fig.  1.  Seesaw movement of tectonic subsidence via a fulcrum

      图  2  SEDPA K层序模拟参数

      Fig.  2.  Input parameter s used in SEDP AK simula tions

      图  3  盆地两侧同期层序同步和非同步叠加模式(模拟参数: “跷跷板”式构造沉降运动、海平面正弦变化曲线)

      Fig.  3.  Synchronous and non-synchro nous stacking patterns of iso chronous sequences in a basin during a sinuous sealevel variation and a seesaw tectonic movement

      图  4  盆地两侧同期层序同步和非同步叠加模式(海平面正弦变化曲线的条件下)

      Fig.  4.  Synchro nous and non-synchronous stacking patterns of isochro nous sequences in a basin during the sinuous change of sea level

      图  5  盆地两侧同期层序同步和非同步叠加模式(均一构造沉降、海平面静止的条件下, 盆地两侧沉积物供应量不同)

      Fig.  5.  Synchronous and non-synchro nous stacking patterns of isochronous sequences in a basin during base level static, symmetrical tectonic subsidence, and variant sediment supplies

      图  6  盆地两侧同期层序同步和非同步叠加模式(不发生构造沉降条件下, 海平面持续上升, 盆地两侧沉积物供应量不同)

      Fig.  6.  Synchronous and non-synchronous stacking patterns of isochronous sequences in a basin during a rise in base level, variant sediment supplies but no tectonic subsidence

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    出版历程
    • 收稿日期:  2008-12-20
    • 刊出日期:  2009-09-25

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