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    渤海走滑断裂对古近系源-汇体系的控制作用

    徐长贵 加东辉 宛良伟

    徐长贵, 加东辉, 宛良伟, 2017. 渤海走滑断裂对古近系源-汇体系的控制作用. 地球科学, 42(11): 1871-1882. doi: 10.3799/dqkx.2017.118
    引用本文: 徐长贵, 加东辉, 宛良伟, 2017. 渤海走滑断裂对古近系源-汇体系的控制作用. 地球科学, 42(11): 1871-1882. doi: 10.3799/dqkx.2017.118
    Xu Changgui, Jia Donghui, Wan Liangwei, 2017. Control of the Strike-Slip Fault to the Source-to-Sink System of the Paleogene in Bohai Sea Area. Earth Science, 42(11): 1871-1882. doi: 10.3799/dqkx.2017.118
    Citation: Xu Changgui, Jia Donghui, Wan Liangwei, 2017. Control of the Strike-Slip Fault to the Source-to-Sink System of the Paleogene in Bohai Sea Area. Earth Science, 42(11): 1871-1882. doi: 10.3799/dqkx.2017.118

    渤海走滑断裂对古近系源-汇体系的控制作用

    doi: 10.3799/dqkx.2017.118
    基金项目: 

    国家科技"十三五"重大专项 2016ZX05024-003

    详细信息
      作者简介:

      徐长贵(1971-), 男, 教授级高级工程师, 博士, 中国海洋石油总公司勘探专家, 主要从事石油地质与综合勘探研究

    • 中图分类号: P618.13

    Control of the Strike-Slip Fault to the Source-to-Sink System of the Paleogene in Bohai Sea Area

    • 摘要: 走滑断裂在渤海海域广泛分布,深刻影响着沉积盆地的形成与演化,同时也深刻影响着源-汇体系的形成和演化.在对渤海海域大量钻井资料和地震资料分析的基础上,认为走滑断裂对渤海古近系源-汇体系的控制作用主要表现在:走滑断裂压扭作用控制了局部物源体系的形成;走滑断裂的张扭作用控制了沟谷低地的形成;走滑断裂的水平运动控制源-汇体系的横向迁移.走滑断裂带源-汇体系发育模式十分复杂,渤海古近系常见的主要有S型走滑断裂带源-汇体系模式、叠覆型走滑断裂带源-汇体系模式、帚状走滑断裂带源-汇体系模式、共轭走滑带源-汇体系模式.开展走滑断裂带源-汇体系特征及其控砂模式的探讨,对含油气盆地的储层预测具有重要的意义.

       

    • 图  1  渤海海域区域地质图与走滑断裂分布

      Fig.  1.  Regional geological map of Bohai sea area and strike-slip faults distrubution map

      图  2  渤海海域走滑断裂带应力发育模式

      a.右旋S型走滑断裂;b.左旋S型走滑断裂;c.右旋帚状走滑断裂;d.左旋帚状走滑断裂;e.右旋叠覆型走滑断裂;f.左旋叠覆型走滑断裂;g.右旋双重型走滑断裂;h.左旋双重型走滑断裂;i.共轭型走滑断裂

      Fig.  2.  Stress mode of strike-slip fault zones in Bohai sea area

      图  3  锦州20-3地区右旋左阶S型走滑断裂控制的局部物源与近源辫状三角洲沉积

      Fig.  3.  The local provenance and proximal braided river delta controlled by dextral left step strike slip fault in JZ20-3 area

      图  4  渤中34-9油田右旋右阶叠覆型走滑断裂控制的沟谷低地与辫状河三角洲沉积

      Fig.  4.  Valley and proximal braided river delta controlled by dextral right step strike slip fault in BZ34-9 oilfield

      图  5  金县1-1地区走滑断裂水平位移与辫状河三角洲“鱼跃式”迁移

      Fig.  5.  Horizontal displacements of strike slip fault and braided river delta fish jumping migrate in JX1-1 area

      图  6  辽东凸起中北段S型走滑带源-汇体系发育模式

      Fig.  6.  type strike slip fault source sink system mode in the middle-north section of Liaodong uplift

      图  7  锦州25-1地区叠覆型走滑断裂带源-汇体系发育模式

      T4代表沙二段顶面;T5代表沙二段底面

      Fig.  7.  En echelon type strike slip fault source sink system mode in JZ25-1 area

      图  8  辽西低凸起北段锦州20-2北地区帚状走滑带源-汇体系发育模式

      Fig.  8.  Brush strike slip fault source sink system mode in JZ20-2N area of the north section of Liaoxi low uplift

      图  9  曹妃甸6-4油田共轭走滑带源-汇体系发育模式

      Fig.  9.  Conjugate strike slip fault source sink system mode in CFD6-4 oilfield

      图  10  走滑断裂带源-汇控砂模式在旅大16-3油田应用

      Fig.  10.  Application of the strike slip fault zone source sink system and its sand control pattern in the LD16-3 oilfield

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    • 收稿日期:  2017-05-06
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