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南海北部陆坡深水区沉积物输送模式探讨

袁圣强 吴时国 赵宗举 徐方建

袁圣强, 吴时国, 赵宗举, 徐方建. 南海北部陆坡深水区沉积物输送模式探讨[J]. 海洋地质与第四纪地质, 2010, 30(4): 39-48. doi: 10.3724/SP.J.1140.2010.04039
引用本文: 袁圣强, 吴时国, 赵宗举, 徐方建. 南海北部陆坡深水区沉积物输送模式探讨[J]. 海洋地质与第四纪地质, 2010, 30(4): 39-48. doi: 10.3724/SP.J.1140.2010.04039
YUAN Shengqiang, WU Shiguo, ZHAO Zongju, XU Fangjian. DEEPWATER SEDIMENT TRANSPORTATION MODELS FOR NORTHERN SOUTH CHINA SEA SLOPES[J]. Marine Geology & Quaternary Geology, 2010, 30(4): 39-48. doi: 10.3724/SP.J.1140.2010.04039
Citation: YUAN Shengqiang, WU Shiguo, ZHAO Zongju, XU Fangjian. DEEPWATER SEDIMENT TRANSPORTATION MODELS FOR NORTHERN SOUTH CHINA SEA SLOPES[J]. Marine Geology & Quaternary Geology, 2010, 30(4): 39-48. doi: 10.3724/SP.J.1140.2010.04039

南海北部陆坡深水区沉积物输送模式探讨


doi: 10.3724/SP.J.1140.2010.04039
详细信息
    作者简介:

    袁圣强(1982-),男,博士后,主要从事沉积储层研究,E-mail:swu@ms.qdio.ac.cn

  • 基金项目:

    国家重点基础研究发展规划项目(2009CB219406)

    中国科学院重要方向性项目(KZCX2-YW-229)

  • 中图分类号: P736.2

DEEPWATER SEDIMENT TRANSPORTATION MODELS FOR NORTHERN SOUTH CHINA SEA SLOPES

More Information
  • 摘要: 南海北部陆坡深水区沉积物输送模式复杂多样,研究发现主要有碎屑流、浊流、砂质碎屑流、碳酸盐岩重力流、块体搬运、河流搬运、深水水道搬运7种类型,它们共同影响着南海北部陆坡沉积物类型和储层分布。其中(砂质)碎屑流沉积、块体搬运沉积、河流供给、深水水道砂是南海北部深水储层的主要成因,而纯粹的浊积岩在该地区发育不广泛。珠江口盆地的深水储层受到河流的供给和后期流体改造的影响,并且存在碳酸盐岩重力流沉积物薄层,证明该地区水动力条件较强;琼东南盆地深水储层分布受到了碎屑流控制和深水水道的影响,相对浅水区来看可能存在分选较好、干净的砂体储层,具有良好的勘探潜力。
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  • 收稿日期:  2010-07-10
  • 修回日期:  2010-07-20

南海北部陆坡深水区沉积物输送模式探讨

doi: 10.3724/SP.J.1140.2010.04039
    作者简介:

    袁圣强(1982-),男,博士后,主要从事沉积储层研究,E-mail:swu@ms.qdio.ac.cn

基金项目:

国家重点基础研究发展规划项目(2009CB219406)

中国科学院重要方向性项目(KZCX2-YW-229)

  • 中图分类号: P736.2

摘要: 南海北部陆坡深水区沉积物输送模式复杂多样,研究发现主要有碎屑流、浊流、砂质碎屑流、碳酸盐岩重力流、块体搬运、河流搬运、深水水道搬运7种类型,它们共同影响着南海北部陆坡沉积物类型和储层分布。其中(砂质)碎屑流沉积、块体搬运沉积、河流供给、深水水道砂是南海北部深水储层的主要成因,而纯粹的浊积岩在该地区发育不广泛。珠江口盆地的深水储层受到河流的供给和后期流体改造的影响,并且存在碳酸盐岩重力流沉积物薄层,证明该地区水动力条件较强;琼东南盆地深水储层分布受到了碎屑流控制和深水水道的影响,相对浅水区来看可能存在分选较好、干净的砂体储层,具有良好的勘探潜力。

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