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    南堡凹陷高柳及四号构造带沙一段-东营组扇体的精细刻画及其成因机制

    李潇鹏 王华 甘华军 马乾 陈思 赵忠新 彭钰会

    李潇鹏, 王华, 甘华军, 马乾, 陈思, 赵忠新, 彭钰会, 2020. 南堡凹陷高柳及四号构造带沙一段-东营组扇体的精细刻画及其成因机制. 地球科学, 45(4): 1295-1307. doi: 10.3799/dqkx.2019.093
    引用本文: 李潇鹏, 王华, 甘华军, 马乾, 陈思, 赵忠新, 彭钰会, 2020. 南堡凹陷高柳及四号构造带沙一段-东营组扇体的精细刻画及其成因机制. 地球科学, 45(4): 1295-1307. doi: 10.3799/dqkx.2019.093
    Li Xiaopeng, Wang Hua, Gan Huajun, Ma Qian, Chen Si, Zhao Zhongxin, Peng Yuhui, 2020. Identification and Formation Mechanism of Fans Developed in 1st Member of Shahejie and Dongying Formations, Gaoliu and No.4 Tectonic Belt, Nanpu Sag. Earth Science, 45(4): 1295-1307. doi: 10.3799/dqkx.2019.093
    Citation: Li Xiaopeng, Wang Hua, Gan Huajun, Ma Qian, Chen Si, Zhao Zhongxin, Peng Yuhui, 2020. Identification and Formation Mechanism of Fans Developed in 1st Member of Shahejie and Dongying Formations, Gaoliu and No.4 Tectonic Belt, Nanpu Sag. Earth Science, 45(4): 1295-1307. doi: 10.3799/dqkx.2019.093

    南堡凹陷高柳及四号构造带沙一段-东营组扇体的精细刻画及其成因机制

    doi: 10.3799/dqkx.2019.093
    基金项目: 

    国家油气重大专项 2016ZX05006-006-002

    详细信息
      作者简介:

      李潇鹏(1989-), 男, 博士研究生, 从事层序地层学及沉积学研究

      通讯作者:

      王华

    • 中图分类号: P512.2

    Identification and Formation Mechanism of Fans Developed in 1st Member of Shahejie and Dongying Formations, Gaoliu and No.4 Tectonic Belt, Nanpu Sag

    • 摘要: 准层序组格架下扇体的精细刻画对于揭示陆相断陷湖盆内部沉积充填演化历史、沉积与构造活动等的耦合关系等具有重要意义,同时,也可为老油区的深入挖潜、细化勘探提供重要参考.利用岩心、测录井及三维地震资料,对南堡凹陷高柳及四号构造带沙一段-东营组的扇体演化特征、扇体形态、结构和成因机制进行研究.结果表明,从时空演化上,沙一段沉积期高柳地区扇体发育程度高,多位于中西部,到东营组沉积期4号构造带扇体发育规模逐渐增大.以外部形态和内部结构为依据,可将发育扇体划分为4个类型,分别为:(1)"外宽内窄",平原河道稳定多分支,前缘河口坝靠近平原,在边界断裂断陷强度高于湖盆中沉降速率的背景下形成;(2)"外窄内宽",平原河道少分支,河口坝数量多,单个规模小,在有逆牵引背斜区发育;(3)长条状,平原河道少分支,前缘河道不稳定,河口坝数量多,铺开面积大,在湖盆沉降速率高于边界断裂断陷速率背景下形成;(4)"鸟足状",平原河道稳定,前缘河道多分支,河口坝数量少,单个规模大,在边界断陷速率与湖盆沉降速率相当的背景下形成.构造古地貌的差异性对扇体形态、内部结构的变化起到了重要的控制作用.

       

    • 图  1  南堡凹陷构造纲要图(a), 充填演化序列图(b)和构造格架剖面图(c)

      图b据王观宏(2016)

      Fig.  1.  Geological map (a), stratigraphic chart (b), and structural framework (c) of Nanpu sag

      图  2  高21井典型沉积亚相演化区段岩心、测井特征柱状图

      平面位置见图 1a

      Fig.  2.  Cores, and wireline log features of the sedimentary facies showing the changing of sub-facies in well Gao 21

      图  3  过高21井顺物源方向典型沉积亚相演化区段地震相差异分析

      平面位置见图 1a

      Fig.  3.  The differences of seismic facies for different sub-facies along the provenance direction across well Gao 21

      图  4  高柳地区连井沉积特征分析

      图中GR的单位为API; SP的单位为mV; 深度的单位为m.平面位置见图 1a

      Fig.  4.  Sedimentary correlation panel in Gaoliu tectonic belt

      图  5  利用地震属性刻画扇体平面展布特征流程

      Fig.  5.  The flow chart of the approach for identifying fans basing on seismic attribute

      图  6  准层序组识别流程图

      井位及剖面位置见图 1a

      Fig.  6.  Flow chart of the approach for building the para-sequence framework

      图  7  不同准层序扇体展布演化图

      Fig.  7.  Evolution features of fans in different para-sequences

      图  8  扇体形态及内部结构对比分析

      Fig.  8.  Comparison chart of the shapes and internal architectures of fans in different types

      图  9  不同类型扇体发育机制及实例分析

      Fig.  9.  Formation mechanism and examples for different types of fans

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