尼日尔三角洲盆地深水沉积的二元结构特征及层序划分
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Characters of Two-Component Constitution of Deep-water Deposit And Sequence Stratigraphy Divided In Niger Delta Basin
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    摘要:

    本文根据测井曲线及地震相特征,建立了深水层序界面划分的5种判别标准,将尼日尔三角洲盆地深水区中中新统-上中新统地层划分了6个三级层序,2个二级层序。根据深水沉积自身沉积旋回所具有的二元结构特征及三角洲与陆架区相对海平面变化之间的关系,将经典的三分体系域划分为二分体系域:异地沉积体系域和原地沉积体系域。其中,异地沉积体系域从基准面下降开始-海侵早期,主要发育重力流沉积(块状搬运沉积、浊积扇);原地沉积体系域从海侵中、晚期-基准面上升最大位置结束,主要以原地沉降的泥质披覆沉积为主。分析了层序发育的影响因素,综合研究认为:气候条件、海平面变化、构造抬升、沉积物供给、大陆架宽窄等共同制约了研究区深水沉积层序的发育。

    Abstract:

    Base on bore logs and seismic facies characters,the article establishs five criterias for judging sequence boundary of deep-water setting, and then the strata of middle-upper Miocene are divided into six third-order sequences, two second-order sequences in Nigeria deep-water setting areas. Base on two-component Constitution feature of deep-water depositional cycle, deltas and relative sea-level change in shelf area, Classic threefold division of systems tracts are classified as twofold division of systems tracts: allogenetic systems tract and autogenetic systems tract. Allogenetic systems tract starts from base level descending to early stage of transgression, and it mainly has gravity current deposits that are composed of mass transport deposits and turbidite fans. Autogenetic systems tract starts from middle-late stage of transgression to base level rising to the highest position, it mainly deposits pelagic and hemipelagic argillaceous sediments.And we also analysis controlled factors of sequence stratigraphy development, but due to the limited datum, it is difficult to predicate that one or even more factors determine sequence development for most sequences.

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王振奇.2013.尼日尔三角洲盆地深水沉积的二元结构特征及层序划分[J].地质学报,87(8):1149-1157.
wang zhenqi.2013. Characters of Two-Component Constitution of Deep-water Deposit And Sequence Stratigraphy Divided In Niger Delta Basin[J]. Acta Geologica Sinica,87(8):1149-1157.

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历史
  • 收稿日期:2012-03-31
  • 最后修改日期:2012-07-02
  • 录用日期:2013-09-11
  • 在线发布日期: 2013-09-16