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南海北部陆坡白云深水区浅层深水水道沉积

刘军 庞雄 颜承志 柳保军 李元平 胡琏 郑金云

刘军, 庞雄, 颜承志, 柳保军, 李元平, 胡琏, 郑金云. 南海北部陆坡白云深水区浅层深水水道沉积[J]. 石油实验地质, 2011, 33(3): 255-259. doi: 10.11781/sysydz201103255
引用本文: 刘军, 庞雄, 颜承志, 柳保军, 李元平, 胡琏, 郑金云. 南海北部陆坡白云深水区浅层深水水道沉积[J]. 石油实验地质, 2011, 33(3): 255-259. doi: 10.11781/sysydz201103255
Liu Jun, Pang Xiong, Yan Chengzhi, Liu Baojun, Li Yuanping, Hu Lian, Zheng Jinyun. Shallow deepwater channels in Baiyun deepwater region of northern continental slope, South China Sea[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(3): 255-259. doi: 10.11781/sysydz201103255
Citation: Liu Jun, Pang Xiong, Yan Chengzhi, Liu Baojun, Li Yuanping, Hu Lian, Zheng Jinyun. Shallow deepwater channels in Baiyun deepwater region of northern continental slope, South China Sea[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(3): 255-259. doi: 10.11781/sysydz201103255

南海北部陆坡白云深水区浅层深水水道沉积

doi: 10.11781/sysydz201103255
基金项目: 国家科技重大专项(2008ZX05025-003,2008ZX05056-001,2008ZX05025-006-03,2008ZX05025-001-010)资助
详细信息
    作者简介:

    刘军(1978- ),男,博士,从事石油地质和油气勘探研究工作.E-mail:liujun5@cnooc.com.cn.

  • 中图分类号: TE121.3

Shallow deepwater channels in Baiyun deepwater region of northern continental slope, South China Sea

  • 摘要: 应用分辨率高的浅层三维地震资料,对白云深水区浅层深水水道沉积系统进行研究,以此指导地震分辨率降低的中深层勘探。在白云凹陷浅层的陆坡、陆坡底都发育大量深水水道,按成因可分为3类:侵蚀型、侵蚀/加积型和加积型。深水水道的几何形态随地形坡度的变化而变化,在上陆坡发育单一的深切供应水道,在坡度较缓的限制性环境内,多个较宽浅的水道垂向叠加,在盆底的非限制性环境,多个小型水道侧向迁移。在平面上,水道形态既有顺直型也有弯曲型。白云凹陷侵蚀/加积型水道垂向变化特征表现为粒度整体向上变细,底部为主水道,顶部为有堤水道。深水水道砂岩的勘探具有复杂性,因此找到厚度大、连通性好的水道砂岩尤为重要。

     

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出版历程
  • 收稿日期:  2010-07-06
  • 修回日期:  2011-04-08
  • 刊出日期:  2011-06-28

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