南海北部中—深层环流格局下海山-阶地-峡谷沉积效应

苏明, 王艺璇, 陈慧, 刘姗, 解习农, 张小波, 常景龙, 孟凡盛, 周海涛, 栾坤祥, 卓海腾, 王策, 雷亚平. 南海北部中—深层环流格局下海山-阶地-峡谷沉积效应[J]. 海洋地质与第四纪地质, 2023, 43(3): 61-73. doi: 10.16562/j.cnki.0256-1492.2023052201
引用本文: 苏明, 王艺璇, 陈慧, 刘姗, 解习农, 张小波, 常景龙, 孟凡盛, 周海涛, 栾坤祥, 卓海腾, 王策, 雷亚平. 南海北部中—深层环流格局下海山-阶地-峡谷沉积效应[J]. 海洋地质与第四纪地质, 2023, 43(3): 61-73. doi: 10.16562/j.cnki.0256-1492.2023052201
SU Ming, WANG Yixuan, CHEN Hui, LIU Shan, XIE Xinong, ZHANG Xiaobo, CHANG Jinglong, MENG Fansheng, ZHOU Haitao, LUAN Kunxiang, ZHUO Haiteng, WANG Ce, LEI Yaping. Depositional mode for the seamount-terrace-canyon sedimentary combination under the impacts of intermediate and deep circulation dynamics in the northern margin of the South China Sea[J]. Marine Geology & Quaternary Geology, 2023, 43(3): 61-73. doi: 10.16562/j.cnki.0256-1492.2023052201
Citation: SU Ming, WANG Yixuan, CHEN Hui, LIU Shan, XIE Xinong, ZHANG Xiaobo, CHANG Jinglong, MENG Fansheng, ZHOU Haitao, LUAN Kunxiang, ZHUO Haiteng, WANG Ce, LEI Yaping. Depositional mode for the seamount-terrace-canyon sedimentary combination under the impacts of intermediate and deep circulation dynamics in the northern margin of the South China Sea[J]. Marine Geology & Quaternary Geology, 2023, 43(3): 61-73. doi: 10.16562/j.cnki.0256-1492.2023052201

南海北部中—深层环流格局下海山-阶地-峡谷沉积效应

  • 基金项目: 广东省基础与应用基础研究基金自然科学基金面上项目(2023A1515010967);国家自然科学基金面上项目(42130408,41976067);南方海洋科学与工程广东省实验室(珠海)资助项目(SML2021SP009);“中山大学”号海洋综合科考实习船科考设备验收航次;南方海洋科学与工程广东省实验室(珠海)南海西边界流大气-海洋-海底-生物综合调查航次
详细信息
    作者简介: 苏明(1982—),男,博士,主要从事海洋地质研究,E-mail:suming3@mail.sysu.edu.cn
    通讯作者: 苏明(1982—),男,博士,主要从事海洋地质研究,E-mail:suming3@mail.sysu.edu.cn
  • 中图分类号: P736.1

Depositional mode for the seamount-terrace-canyon sedimentary combination under the impacts of intermediate and deep circulation dynamics in the northern margin of the South China Sea

More Information
  • 作为研究水-岩界面物质能量交换的天然实验室,南海北缘陆坡区具有复杂的地形地貌(如凸起海山、平坦阶地、下凹峡谷等),并发育不同类型的深水沉积体系(包括重力流滑移滑塌、浊流和底流沉积等)。基于高分辨率海底地形、地震反射资料,海水温盐深(CTD)观测资料,以及已发表的海洋沉积学及物理海洋数值模拟结果,本文针对南海北缘代表型陆坡区开展中—深层环流格局下海山-阶地-峡谷沉积效应分析。发现了尖峰陆坡区侵蚀型-海山型(环槽-丘状漂积体)和席状/无沉积型底流阶地的沉积组合,以及一统陆坡区海山相关底流沉积(环槽-丘状漂积体)-席状/无沉积型底流阶地-黏附型漂积体-陡坡滑塌/峡谷体系的沉积组合;揭示了这些典型深水沉积组合与南海中—深层环流动力格局的耦合关系。该成果对于深入了解深水沉积过程对中-深层动力格局的响应及其对于大陆边缘形态的塑造具有较好的启示意义。

  • 加载中
  • 图 1  基于海底几何形状和底层结构识别的各种侵蚀、无沉积和沉积特征

    Figure 1. 

    图 2  南海北部陆缘综合概况图(a)和过尖峰陆坡东沙南海山综合剖面图(b)

    Figure 2. 

    图 3  尖峰陆坡东沙南海山附近深水沉积体系分布图(左)及坡度图(右)

    Figure 3. 

    图 4  一统陆坡东沙南海山附近深水沉积体系分布图(左)及坡度图(右)

    Figure 4. 

    图 5  中-深层环流格局下海山-阶地-峡谷沉积效应模式图

    Figure 5. 

    表 1  物理海洋CTD观测站位信息

    Table 1.  Information of CTD stations

    站位号位置CTD最大采水深度/m
    S120.059°N 、117.424°E208
    S220.006°N 、117.573°E1 791
    T119.619°N 、114.150°E544
    T219.024°N 、114.424°E1 604
    下载: 导出CSV
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出版历程
收稿日期:  2023-05-22
修回日期:  2023-06-20
刊出日期:  2023-06-28

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