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    琼东南盆地深水区构造格局和幕式演化过程

    雷超 任建业 裴健翔 林海涛 尹新义 佟殿君

    雷超, 任建业, 裴健翔, 林海涛, 尹新义, 佟殿君, 2011. 琼东南盆地深水区构造格局和幕式演化过程. 地球科学, 36(1): 151-162. doi: 10.3799/dqkx.2011.016
    引用本文: 雷超, 任建业, 裴健翔, 林海涛, 尹新义, 佟殿君, 2011. 琼东南盆地深水区构造格局和幕式演化过程. 地球科学, 36(1): 151-162. doi: 10.3799/dqkx.2011.016
    LEI Chao, REN Jian-ye, PEI Jian-xiang, LIN Hai-tao, YIN Xin-yi, TONG Dian-jun, 2011. Tectonic Framework and Multiple Episode Tectonic Evolution in Deepwater Area of Qiongdongnan Basin, Northern Continental Margin of South China Sea. Earth Science, 36(1): 151-162. doi: 10.3799/dqkx.2011.016
    Citation: LEI Chao, REN Jian-ye, PEI Jian-xiang, LIN Hai-tao, YIN Xin-yi, TONG Dian-jun, 2011. Tectonic Framework and Multiple Episode Tectonic Evolution in Deepwater Area of Qiongdongnan Basin, Northern Continental Margin of South China Sea. Earth Science, 36(1): 151-162. doi: 10.3799/dqkx.2011.016

    琼东南盆地深水区构造格局和幕式演化过程

    doi: 10.3799/dqkx.2011.016
    基金项目: 

    国家重点基础研究发展规划"973"项目 2007CB41170502

    国家自然科学基金 40672089

    博士点基金 20070491004

    2009年美国石油地质学家学会研究生科研基金 AAPG-In-Grant

    详细信息
      作者简介:

      雷超(1984-), 男, 博士研究生, 主要从事沉积盆地动力学及其能源效应研究.E-mail: chaolei@hotmail.com

    • 中图分类号: P618

    Tectonic Framework and Multiple Episode Tectonic Evolution in Deepwater Area of Qiongdongnan Basin, Northern Continental Margin of South China Sea

    • 摘要: 基于大量琼东南盆地深水区高精度的地质-地球物理和钻井资料解释, 确立了该盆地"南北分带, 东西分块"的基本构造格局; 通过构造-地层、沉降史和沉降中心厘定等方面的综合研究, 在琼东南深水盆地中深入描述和分析了T70重要的构造变革界面特征, 该界面之下发育了一系列分散的、NE向展布的小型断陷盆地群, 该界面之上一直到T60界面发育时期, 盆地的沉降中心逐渐迁移到位于琼东南盆地中央坳陷区的、呈NE-WE-NWW弧形展布的大型断坳式盆地内, 该断坳盆地与下伏小型断陷盆地群构成显著的叠加关系; 以控盆边界断层的性质和几何学分布, 确定下伏的NE向展布的小型断陷盆地群受控于NW-SE向拉伸应力场, 而上覆的断坳盆地由近SN向拉伸应力作用所形成; 区域对比表明该界面广泛分布于南海北部大陆边缘盆地中, 具有区域性分布的特征; 生物地层和区域对比表明该界面年龄为32 Ma, 与南海初始扩张的年龄一致.因此, 该界面是一个发育于南海北部的、代表了南海扩张开始的一个区域性构造变革界面.该界面的发育导致了琼东南盆地深水区盆地结构和构造演化的复杂性, 以该界面为基础, 结合盆地充填序列中的其他重要界面和盆地的沉降史分析, 将盆地的构造演化划分为断陷、断坳、裂后热沉降和加速沉降4个构造演化幕, 从而确定了该盆地具有典型的幕式演化特征; 详细讨论了盆地周缘板块运动学重组事件和岩石圈深部活动对琼东南盆地幕式发育过程的控制机制.

       

    • 图  1  琼东南盆地区域地质背景及其构造单元划分

      图 1a为琼东南盆地所处区域背景;图 1b为琼东南盆地构造格架图;图 1c图 1b中L3地震解释剖面;图 1d为盆地“东西分块”构造转换带“堑垒”构造样式特征;图中L1、L2…L6为图 1图 3地震剖面平面位置

      Fig.  1.  Regional geological setting and its tectonic unit division of QDNB

      图  2  琼东南盆地地层发育特征及其动力学背景

      Fig.  2.  Characteristics of strata and their dynamical setting of QDNB

      图  3  盆地过主要构造单元地震剖面构造-地层解释

      Fig.  3.  Seismic reflection profiles across main tectonic units of QDNB and their tectono-stratigraphic interpretation

      图  4  琼东南盆地不同时期断层发育特征及其控制凹陷简化

      Fig.  4.  Simplified maps of distribution of faults and associated depressions in different episode in QDNB

      图  5  琼东南盆地主要凹陷总沉降特征

      Fig.  5.  Subsidence characteristics of main depression in QDNB

      图  6  不同时期琼东南盆地沉降中心

      Fig.  6.  Subsidence centers of different episode in QDNB

      图  7  东南亚盆地形成演化模式(据Tapponnier et al.(1982)Lee and Lawver(1995)Morley(2002)Clift et al.(2008)Hall(2002)Hall et al.(2008)Fyhn et al.(2009)资料编绘)

      Fig.  7.  Schematic figures showing evolution of sedimentary basins in Southeast Asia

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