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    琼东南华光凹陷深水重力搬运沉积体系及其油气勘探

    姚根顺 袁圣强 马玉波 秦蕴珊 吴时国

    姚根顺, 袁圣强, 马玉波, 秦蕴珊, 吴时国, 2009. 琼东南华光凹陷深水重力搬运沉积体系及其油气勘探. 地球科学, 34(3): 471-476.
    引用本文: 姚根顺, 袁圣强, 马玉波, 秦蕴珊, 吴时国, 2009. 琼东南华光凹陷深水重力搬运沉积体系及其油气勘探. 地球科学, 34(3): 471-476.
    YAO Gen-shun, YUAN Sheng-qiang, MA Yu-bo, QIN Yun-shan, WU Shi-guo, 2009. Deepwater Mass Transport Deposition System of Huaguang Depression, Qiongdongnan Basin and Its Significance for Hydrocarbon Exploration. Earth Science, 34(3): 471-476.
    Citation: YAO Gen-shun, YUAN Sheng-qiang, MA Yu-bo, QIN Yun-shan, WU Shi-guo, 2009. Deepwater Mass Transport Deposition System of Huaguang Depression, Qiongdongnan Basin and Its Significance for Hydrocarbon Exploration. Earth Science, 34(3): 471-476.

    琼东南华光凹陷深水重力搬运沉积体系及其油气勘探

    基金项目: 

    中国科学院三期院创新重要方向项目 KZCX2-YW-229

    中国科学院三期院创新重要方向项目 KZCX2-YW-203

    国家重点基础研究发展计划项目课题 2007CB411703

    详细信息
      作者简介:

      姚根顺(1962-), 男, 教授级高级工程师, 主要从事碳酸盐岩和深水油气地质相关研究.E-mail:yaogs_hz@petrochina.com.cn

    • 中图分类号: P618

    Deepwater Mass Transport Deposition System of Huaguang Depression, Qiongdongnan Basin and Its Significance for Hydrocarbon Exploration

    • 摘要: 重力搬运沉积作用形成的岩性地层圈闭对深水油气勘探具有非常重要的作用.为弄清琼东南盆地华光凹陷重力搬运沉积特征, 基于近年新采集的地震资料和经典层序地层模式, 开展了该区的深水沉积特征研究.南海西北部深水区重力搬运沉积特征发育, 主要包括中新统三亚组发育的复合水道、上新统变形滑坡体及第四系深水浊积水道.三亚组复合水道具有典型的强弱振幅相互叠置特征, 上新统变形滑坡体具有典型的下部变形、上部滑坡的双层结构, 第四系深水浊积水道具有典型的侧向迁移、分支水道等特征.这些沉积特征的形成与越南隆起的物源供给有关.复合水道充填可作为潜在的深水储层, 滑塌体的形成可能与天然气水合物的形成或解体有关.

       

    • 图  1  研究区构造位置及水深分布

      Fig.  1.  Structural location and bathgram map of study area

      图  2  水道形成期次图示

      (据Navarre et al.,2002修改)

      Fig.  2.  Paradigm of channel

      图  3  过复合水道的N-S走向剖面及其解释图

      (位置见图 1)

      Fig.  3.  N-S trend seismic profile and interpretation map across the channel complex of Sanya Formation

      图  4  过滑坡体的E-W走向(a)和SN走向(b)剖面及其解释图

      (位置见图 1)

      Fig.  4.  E-W trend (a) and SN (b) seismic profile and interpretation map across the slide

      图  5  相干时间切片显示深水水道的平面特征

      (位置见图 1)

      Fig.  5.  Coherence time-slice shows the plane characteris- tics of deepwater channels

      图  6  过第四系水道的两条地震剖面

      (位置见图 5)

      Fig.  6.  Seismic profiles across the Quaternary deepwater channels

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    • 收稿日期:  2008-11-10
    • 刊出日期:  2009-05-25

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