珠江口盆地西部文昌A凹陷断裂特征与成因探讨

张豪, 栾锡武, 冉伟民, 王阔, 魏新元, 石艳锋, MohammadSaiful Islam, 王嘉. 珠江口盆地西部文昌A凹陷断裂特征与成因探讨[J]. 海洋地质与第四纪地质, 2020, 40(4): 96-106. doi: 10.16562/j.cnki.0256-1492.2019050901
引用本文: 张豪, 栾锡武, 冉伟民, 王阔, 魏新元, 石艳锋, MohammadSaiful Islam, 王嘉. 珠江口盆地西部文昌A凹陷断裂特征与成因探讨[J]. 海洋地质与第四纪地质, 2020, 40(4): 96-106. doi: 10.16562/j.cnki.0256-1492.2019050901
ZHANG Hao, LUAN Xiwu, RAN Weimin, WANG Kuo, WEI Xinyuan, SHI Yanfeng, Mohammad Saiful Islam, WANG Jia. Discussion on fault characteristics and genesis of Wenchang A Sag in the west of the Pearl River Mouth Basin[J]. Marine Geology & Quaternary Geology, 2020, 40(4): 96-106. doi: 10.16562/j.cnki.0256-1492.2019050901
Citation: ZHANG Hao, LUAN Xiwu, RAN Weimin, WANG Kuo, WEI Xinyuan, SHI Yanfeng, Mohammad Saiful Islam, WANG Jia. Discussion on fault characteristics and genesis of Wenchang A Sag in the west of the Pearl River Mouth Basin[J]. Marine Geology & Quaternary Geology, 2020, 40(4): 96-106. doi: 10.16562/j.cnki.0256-1492.2019050901

珠江口盆地西部文昌A凹陷断裂特征与成因探讨

  • 基金项目: 中国东盟海上合作基金项目(12120100500017001);青岛海洋科学与技术试点国家实验室基金项目(QNLM201708);自然资源部公益性行业科研专项基金“海底冷泉拖曳式快速成像系统研制及应用”(201511037);海洋矿产资源评价与探测技术功能实验室开放基金“开平凹陷地区地质与矿产资源勘探”(MMRKF201804);鳌山科技创新项目(2016ASKJ11,2016ASKJ13,2017ASKJ02)
详细信息
    作者简介: 张豪(1994—),男,硕士,研究方向为油气田勘探开发地球物理技术,E-mail:z17010089@s.upc.edu.cn
    通讯作者: 栾锡武(1966—),男,研究员,研究方向为海洋地球物理测量与数据处理方法以及大陆边缘构造演化,E-mail:xluan@qnlm.ac
  • 中图分类号: P736.1

Discussion on fault characteristics and genesis of Wenchang A Sag in the west of the Pearl River Mouth Basin

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  • 在前人勘探解释的基础上,通过三维高分辨率地震资料,应用相干属性分析等技术对区域断裂进行精细化解释。研究表明盆地内发育着典型的犁式、花状构造、旋转正断层等伸展构造样式,在珠三南断裂影响下,南部边界断裂以阶梯状排列形成断阶构造。始新世—中中新世,断裂走向在持续右旋张扭应力场下以NE→EW→NWW顺时针方向旋转,张裂强度逐渐减弱。晚始新世—早渐新世,盆地在太平洋板块俯冲后退、印亚板块碰撞、古南海向南俯冲下发育EW向断裂,晚渐新世在南海扩张事件影响下前期右旋应力场得到加强,形成大量近EW向断裂,中新世后演化为NWW向断裂。文昌A凹陷断裂构造的演化、成因机制与南海北部陆缘应力场变化一致。该研究有利于进一步了解南海北部陆缘含油气盆地的构造特征和演化规律,提高油气勘探开发的效率。

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  • 图 1  珠江口盆地西部珠三坳陷构造单元划分 (据文献[2]修改)

    Figure 1. 

    图 2  珠江口盆地西部综合柱状图 (据文献[4, 12]修改)

    Figure 2. 

    图 3  文昌A凹陷断裂组合类型

    Figure 3. 

    图 4  相干切片及断裂平面组合分布

    Figure 4. 

    图 1 

    图 5  断层活动速率分析

    Figure 5. 

    图 6  地震剖面L1259测线6号断裂

    Figure 6. 

    图 7  断层活动速率图(L1259测线,据文献[19-20]修改)

    Figure 7. 

    图 8  华南陆缘及其周缘构造演化过程(据文献[23-24]修改,PRMB为珠江口盆地)

    Figure 8. 

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出版历程
收稿日期:  2019-05-09
修回日期:  2019-11-26
刊出日期:  2020-08-25

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