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    早‒中中新世古珠江三角洲沉积格局及其控制因素

    彭光荣 杜家元 冯进 丁琳 李智高 李小平

    彭光荣, 杜家元, 冯进, 丁琳, 李智高, 李小平, 2022. 早‒中中新世古珠江三角洲沉积格局及其控制因素. 地球科学, 47(11): 3989-4004. doi: 10.3799/dqkx.2022.390
    引用本文: 彭光荣, 杜家元, 冯进, 丁琳, 李智高, 李小平, 2022. 早‒中中新世古珠江三角洲沉积格局及其控制因素. 地球科学, 47(11): 3989-4004. doi: 10.3799/dqkx.2022.390
    Peng Guangrong, Du Jiayuan, Feng Jin, Ding Lin, Li Zhigao, Li Xiaoping, 2022. Depositional Setting of Ancient Pearl River Delta during Early-to-Middle Miocene: Implications for Forcing Factors. Earth Science, 47(11): 3989-4004. doi: 10.3799/dqkx.2022.390
    Citation: Peng Guangrong, Du Jiayuan, Feng Jin, Ding Lin, Li Zhigao, Li Xiaoping, 2022. Depositional Setting of Ancient Pearl River Delta during Early-to-Middle Miocene: Implications for Forcing Factors. Earth Science, 47(11): 3989-4004. doi: 10.3799/dqkx.2022.390

    早‒中中新世古珠江三角洲沉积格局及其控制因素

    doi: 10.3799/dqkx.2022.390
    基金项目: 

    中海石油(中国)有限公司深圳分公司科研项目 CCL2021SZPS0113

    详细信息
      作者简介:

      彭光荣(1978-),男,硕士,高级工程师,主要从事石油地质与油气勘探综合研究工作. ORCID:0000-0003-2014-4653. E-mail:penggr@cnooc.com.cn

    • 中图分类号: P539.2;P736.2

    Depositional Setting of Ancient Pearl River Delta during Early-to-Middle Miocene: Implications for Forcing Factors

    • 摘要: 古珠江三角洲是珠江口盆地油气勘探的重要目标,但对其总体沉积面貌的揭示仍未充分,在一定程度上限制了对区内有利砂体和潜在岩性圈闭的锁定.本次研究综合利用重矿物、岩心、钻井和区域三维地震数据,采用地震沉积学综合分析手段精确复现了早‒中中新世古珠江三角洲的宏观沉积格局和相带展布.重矿物分析结果显示,古珠江分流河道体系向近端侧主要发源于西侧、东侧两个主河道分支,进而确定了古珠江三角洲“双支主控”的宏观基本格局.此外,经过对这两个分支河道体系重矿物组合特征对比,发现其分别与现代西江、东/北江有一定相似性,这可能表明中新世古珠江干流的流路与现今具有较高对比性.同时,针对分流河道和外缘条带砂的精细地震地貌分析显示出中新世古珠江三角洲可能受到河流‒波浪‒潮汐混合动力过程的影响,并且持续的西南向古水流对整体相带展布也具有明显的控制作用.

       

    • 图  1  研究区位置和珠江流域范围图

      1. 黑潮;2. 黑潮南海分支;3. 广东沿岸流;4. 南海暖流;5. 沿岸流

      Fig.  1.  Location of the study area and map of the Pearl River basin

      图  2  珠江口盆地珠一坳陷构造单元分布、三维工区位置及具有重矿物数据的钻井井位

      Fig.  2.  Location map showing the tectonic elements, 3D-survey locations and well locations with heavy mineral data in Zhu Ⅰ depression, Pearl River Mouth basin

      图  3  珠江口盆地珠一坳陷地层柱状图和层序划分方案

      Fig.  3.  Stratigraphic column and sequence division scheme in Zhu Ⅰ depression, Pearl River Mouth basin

      图  4  珠一坳陷内SW-NE方向关键井联井剖面(剖面位置见图 2

      Fig.  4.  Well correlation of key wells in SW-NE direction in Zhu Ⅰ depression (see location in Fig. 2)

      图  5  珠江口盆地珠一坳陷关键钻井重矿物组合及分布情况

      Fig.  5.  Heavy mineral combination and distribution of key drilling wells in ZhuⅠdepression, Pearl River Mouth basin

      图  6  珠江流域及珠一坳陷珠江组典型样品碎屑锆石年龄谱系对比

      Fig.  6.  Comparison of detrital zircon age spectra in typical samples from Zhujiang Formatin of Zhu I depression and the Pearl River drainage basin

      图  7  珠一坳陷北部SW-NE方向地震剖面(剖面位置见图 2

      Fig.  7.  A regional SW-NE seismic profile across the Zhu I depression (see location in Fig.2)

      图  8  中新世古珠江三角洲典型地震地貌单元的岩心和测井响应特征

      Fig.  8.  Core and well log motifs of typical depositional elements of the Miocene Pearl River delta

      图  9  中新世古珠江三角洲典型地震地貌特征显示出河流‒波浪‒潮汐的混合动力过程

      Fig.  9.  Representative seismic geomorphology of the Miocene Pearl River delta showing a mixed river-wave-tidal-dominated process

      图  10  中新世古珠江三角洲代表性沉积相图(以SQT40层序为例)

      Fig.  10.  Representative sedimentary facies map of the Miocene Pearl River delta (SQT40)

      图  11  中新世古珠江三角洲沉积模式

      Fig.  11.  Depositonal model of the Miocene Pearl River delta

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    • 收稿日期:  2022-06-24
    • 网络出版日期:  2022-12-07
    • 刊出日期:  2022-11-25

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