ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    刘景彦, 曲爱英, 刘元贵, 蔡文杰, 李全, 李涣浦. 辽河东部凹陷红星地区古近系高精度层序地层和沉积体系研究[J]. 西北地质,2008,41(2): 73-80.
    引用本文: 刘景彦, 曲爱英, 刘元贵, 蔡文杰, 李全, 李涣浦. 辽河东部凹陷红星地区古近系高精度层序地层和沉积体系研究[J]. 西北地质,2008,41(2): 73-80.
    LIU Jing-yan, QU Ai-ying, LIU Yuan-gui, CAI Wen-jie, LI Quan, LI Huan-pu. The High-Resolution Sequence Stratigraphy and Depositional System Study of Eogene Hongxing Area, Eastern Depression of Liaohe[J]. Northwestern Geology,2008,41(2): 73-80.
    Citation: LIU Jing-yan, QU Ai-ying, LIU Yuan-gui, CAI Wen-jie, LI Quan, LI Huan-pu. The High-Resolution Sequence Stratigraphy and Depositional System Study of Eogene Hongxing Area, Eastern Depression of Liaohe[J]. Northwestern Geology,2008,41(2): 73-80.

    辽河东部凹陷红星地区古近系高精度层序地层和沉积体系研究

    The High-Resolution Sequence Stratigraphy and Depositional System Study of Eogene Hongxing Area, Eastern Depression of Liaohe

    • 摘要: 以高精度层序地层理论为指导,综合大量的钻测井资料和岩心观察,在红星地区古近系沙河街组一段和东营组三段建立了储层规模的高精度层序格架,划分出4个三级层序、19个四级层序和一系列五级层序;测井曲线和岩心观察相结合进行沉积微相分析,识别出扇三角洲前缘和辫状河三角洲前缘水下分流河道、河口坝、前三角洲、决口扇、分流间湾等微相类型;主要储层砂体发育的四级层序沉积体系平面编图表明,不同沉积相或微相无疑是造成砂体形态、分布及储集性变化的直接影响因素.沙一段以扇三角洲前缘水下分流河道或分流河道相储层为主,粒度粗,单一砂层厚度大;而东三段以河流或辫状河三角洲砂体为主,粒度较细,单一砂层较薄.平面上,从北东向南或南西方向显示出从分流河道砂体向三角洲前缘远端坝砂体过渡的变化趋势.沉积相的分布格局控制着砂体类型和分布.

       

      Abstract: Guided by high-resolution sequence stratigraphy theory, combined with lots of logging data and core observation, areservoir-scale high-resolution sequence stratigraphy framework of the Eogene first member of Shahejie for mation and the third member of Dong ying fo rmation has beenest ablished in Hongxing area. 43rd order sequences and 194th order paramsequence sets and series of 5th order paramsequences have been classified in this paper. Acco rding to the logginganalysis and coreobservation, several of sedimentary microfacies of Sha1 and Dong3 have been recognized, such as fandelta front sub-distritary channel, mouth bar, front delta, flooding fan, distributary interval and soon. The depositional systems mapping of 4th order sequence show that different sedimentary microfacies form different sand configuration and distribution and physical characteristic of reservoir. Because fan delta front sub-distributary channel or distribut ary channel is the major depositional microfacies of Sha1, the reser voirmainly is coarsegrade and single thick sand. While braided or braided delta is the major depositional system of Dong3, the reservoir mainly is fine grade and single thin sand. In literally, there shows the evolutiont rend from northeast and southwest distributaries channel sand to delta front far barsand. The distribution configuration of depositional system controlled the sand types and distribution.

       

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