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    渤海古近系混合沉积发育特征与沉积模式

    宋章强 杜晓峰 徐伟 卢欢 陈丽祥

    宋章强, 杜晓峰, 徐伟, 卢欢, 陈丽祥, 2020. 渤海古近系混合沉积发育特征与沉积模式. 地球科学, 45(10): 3663-3676. doi: 10.3799/dqkx.2020.223
    引用本文: 宋章强, 杜晓峰, 徐伟, 卢欢, 陈丽祥, 2020. 渤海古近系混合沉积发育特征与沉积模式. 地球科学, 45(10): 3663-3676. doi: 10.3799/dqkx.2020.223
    Song Zhangqiang, Du Xiaofeng, Xu Wei, Lu Huan, Chen Lixiang, 2020. Sedimentary Features and Development Pattern of Mixed Deposition of Paleogene System in Bohai Sea Area. Earth Science, 45(10): 3663-3676. doi: 10.3799/dqkx.2020.223
    Citation: Song Zhangqiang, Du Xiaofeng, Xu Wei, Lu Huan, Chen Lixiang, 2020. Sedimentary Features and Development Pattern of Mixed Deposition of Paleogene System in Bohai Sea Area. Earth Science, 45(10): 3663-3676. doi: 10.3799/dqkx.2020.223

    渤海古近系混合沉积发育特征与沉积模式

    doi: 10.3799/dqkx.2020.223
    基金项目: 

    国家科技重大专项 2016ZX05024-003

    国家自然科学基金项目 41772111

    详细信息
      作者简介:

      宋章强(1981-), 男, 高级工程师, 主要从事沉积储层研究.ORCID:0000-0002-0009-3982.E-mail:songzhq@cnooc.com.cn

    • 中图分类号: P67

    Sedimentary Features and Development Pattern of Mixed Deposition of Paleogene System in Bohai Sea Area

    • 摘要: 陆源碎屑与湖相碳酸盐混合沉积在渤海海域古近系普遍发育,已经成为重要的油气勘探目标.基于90余口已钻井,结合地震、测井以及相关分析化验资料,以渤海海域古近系钻遇的混合沉积为研究对象,开展了沉积特征与成因背景分析,建立了混合沉积发育模式.研究表明:渤海古近系混合沉积发育近岸混积扇、近岸混积滩坝、远岸混积滩坝3种沉积相、7种沉积亚相和14种沉积微相.近岸混积扇以发育混积沟道为典型特征,岩性为含生屑的砂砾岩或中粗砂岩,为陡坡扇三角洲环境短源水道废弃后与生物碎屑间歇性间互沉积;近岸混积滩坝,为近源搬运沉积的陆源碎屑与盆内碎屑之间的混合沉积,典型沉积特征为发育高陆源碎屑含量的各种粒屑滩或坝;远岸混积滩坝为典型的以富含生物碎屑为主的混合沉积,陆源碎屑含量低,一般为盆内低隆或孤立潜山之上原地生长生物与少量供给的陆源碎屑发生的混合沉积.混合沉积发育模式和规模受古气候与古水体环境、古构造与水动力、陆源碎屑物质供给、古地貌条件等共同控制,其中古地貌特征起主导作用.混合沉积发育模式的建立,对混积型储层预测和油气勘探具有重要意义.

       

    • 图  1  渤海海域构造单元划分与主要混合沉积分布

      Fig.  1.  Tectonic units and distribution of mixed sedimentation of Bohai Sea area

      图  2  渤海海域古近系综合柱状图

      Fig.  2.  Comprehensive diagram indicating Paleogene system of Bohai Sea area

      图  3  近岸混积扇典型特征:Q29-5井为例

      Fig.  3.  Typical features of nearshore mixed fan: taking well Q29-5 for example

      图  4  近岸(湖湾型)混积滩坝典型特征:Q36-2井为例

      Fig.  4.  Typical features of (lake bay) nearshore mixed bar: taking well Q36-2 for example

      图  5  近岸(低隆型)混积滩坝典型特征:B36-W井为例

      Fig.  5.  Typical features of (low uplift) offshore mixed bar: taking well B36-W for example

      图  6  (硬底型)远岸混积滩坝典型特征:J20构造为例

      Fig.  6.  Typical features of (sandy) offshore mixed bar: taking structure J20 for example

      图  7  (软底型)远岸混积滩坝典型发育特征:以Q30构造为例

      Fig.  7.  Typical features of (muddy) offshore mixed bar: taking structure Q30 for example

      图  8  渤海海域秦皇岛地区沙一二段微量元素及气候、水体环境分析

      Fig.  8.  Trace element, climate condition and water environment in Paleogene strata of Qinhuangdao region of Bohai Sea area

      图  9  渤海海域混积岩发育与古地貌特征耦合关系直方图

      Fig.  9.  Diagram reflecting the coupling relationship of mixed sediments development with paleogeomorphic feature in Paleogene strata of Bohai Sea area

      图  10  渤海海域古近系混合沉积发育综合模式

      Fig.  10.  Comprehensive model of Paleogene mixed sediments of Bohai Sea area

      表  1  渤海海域古近系混合沉积相划分

      Table  1.   Sedimentary facies division of the mixed deposits in Paleogene system of Bohai Sea area

      沉积相 亚相 微相 典型岩石类型 主要发育层段 典型构造及取心井
      近岸混积扇 近岸混积扇根 近端沟道 正常沟道沉积的砾岩 沙一二段 Q29-4井
      近岸混积扇中 混积沟道 含生屑砂砾岩 Q29-4井、Q29-5井
      混积碎屑滩 含生屑中-粗粒砂岩 Q29-4井、Q29-5井
      混积生屑(粒屑)滩 含陆屑生屑白云岩 Q29-4井、Q29-5井
      近岸混积扇缘 (含生屑)灰质或云质细-粉砂岩 B27-2井
      近岸混积滩坝 近岸混积坝 砾质混积坝 含生屑砾岩 沙一二段为主,沙三段 L25-2井
      砂质混积坝 含生屑砂岩 L25-2井
      近岸混积滩 混积泥质滩 灰质泥岩 B36-W井
      混积泥晶滩 泥晶灰岩/云岩 B36-W井
      混积生屑(粒屑)滩 含陆屑生屑白云岩 Q36-2井、S36-15井
      混积碎屑滩 含生屑中-粗砂岩 Q36-2井、B36-W井
      远岸混积滩坝 远岸混积坝 砾质混积坝 含生屑砾岩 沙一二段沙四段 C2-2井、J20-1井、J20-2井
      远岸混积滩 混积生屑(粒屑)滩 (含陆屑)生屑白云岩 C2-2井、J20-2井、J20-5、J20-6、B13-2井
      混积碎屑滩 含内碎屑中-粗砂岩 B13-3井
      混积泥晶滩 泥晶灰岩/白云岩 J20-4井、J20-5井、J20-6井
      下载: 导出CSV
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    • 收稿日期:  2020-07-29
    • 刊出日期:  2020-11-17

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