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渤海沙垒田地区新近系明下段多河型地震地貌学特征

谈明轩 朱筱敏 刘强虎 刘伟 李顺利 赵芳

谈明轩, 朱筱敏, 刘强虎, 刘伟, 李顺利, 赵芳. 渤海沙垒田地区新近系明下段多河型地震地貌学特征[J]. 石油实验地质, 2019, 41(3): 411-419. doi: 10.11781/sysydz201903411
引用本文: 谈明轩, 朱筱敏, 刘强虎, 刘伟, 李顺利, 赵芳. 渤海沙垒田地区新近系明下段多河型地震地貌学特征[J]. 石油实验地质, 2019, 41(3): 411-419. doi: 10.11781/sysydz201903411
TAN Mingxuan, ZHU Xiaomin, LIU Qianghu, LIU Wei, LI Shunli, ZHAO Fang. Seismic geomorphological characteristics of multiple fluvial patterns in the Neogene Lower Minghuazhen Member in the Shaleitian area, Bohai Sea[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(3): 411-419. doi: 10.11781/sysydz201903411
Citation: TAN Mingxuan, ZHU Xiaomin, LIU Qianghu, LIU Wei, LI Shunli, ZHAO Fang. Seismic geomorphological characteristics of multiple fluvial patterns in the Neogene Lower Minghuazhen Member in the Shaleitian area, Bohai Sea[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(3): 411-419. doi: 10.11781/sysydz201903411

渤海沙垒田地区新近系明下段多河型地震地貌学特征

doi: 10.11781/sysydz201903411
基金项目: 

国家科技重大专项(2017ZX05001002-002)资助。

详细信息
    作者简介:

    谈明轩(1990-),男,博士研究生,从事层序地层学、沉积学研究。E-mail:mingxuantan0301@hotmail.com。

    通讯作者:

    朱筱敏(1960-),男,教授,博士生导师,从事层序地层学、地震沉积学、储层地质学研究。E-mail:xmzhu@cup.edu.cn。

  • 中图分类号: TE121.31

Seismic geomorphological characteristics of multiple fluvial patterns in the Neogene Lower Minghuazhen Member in the Shaleitian area, Bohai Sea

  • 摘要: 渤海沙垒田地区新近系明化镇组下段主要发育河流相沉积,是渤海地区浅层油气勘探的重点。利用地震地貌学方法结合现代河流体系卫星照片,在重点区的若干典型地层切片中识别出顺直河、中-低弯度曲流河(弯曲度1.2~1.8)及辫状河等多种河流地貌类型,并在明下上亚段沉积阶段发现了辫状河、曲流河共存现象。古沉积坡降分析表明,在整体宽缓的沉积背景下,顺直河、曲流河坡降整体偏小,辫状河坡降相对较大。利用地貌-水动力关系进行古流量估算,认为辫状河满岸流量最大可达3 942 m3/s,曲流河满岸流量最小为145 m3/s,顺直河满岸流量一般小于300 m3/s。基于坡降-流量进行河流类型的判别,可增进对研究区不同河型发育特征、多河型地貌、辫曲共存现象及复杂河道砂体空间展布的认识。

     

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出版历程
  • 收稿日期:  2019-01-03
  • 修回日期:  2019-04-20
  • 刊出日期:  2019-05-28

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