南海西北部莺琼陆坡36.6 ka以来的浊流沉积

许莎莎, 冯秀丽, 冯利, 肖晓, 刘爽

许莎莎, 冯秀丽, 冯利, 肖晓, 刘爽. 南海西北部莺琼陆坡36.6 ka以来的浊流沉积[J]. 海洋地质与第四纪地质, 2020, 40(5): 15-24. DOI: 10.16562/j.cnki.0256-1492.2019112701
引用本文: 许莎莎, 冯秀丽, 冯利, 肖晓, 刘爽. 南海西北部莺琼陆坡36.6 ka以来的浊流沉积[J]. 海洋地质与第四纪地质, 2020, 40(5): 15-24. DOI: 10.16562/j.cnki.0256-1492.2019112701
XU Shasha, FENG Xiuli, FENG Li, XIAO Xiao, LIU Shuang. Turbidite records since 36.6 ka at the Yingqiong continental slope in the northwest of South China Sea[J]. Marine Geology & Quaternary Geology, 2020, 40(5): 15-24. DOI: 10.16562/j.cnki.0256-1492.2019112701
Citation: XU Shasha, FENG Xiuli, FENG Li, XIAO Xiao, LIU Shuang. Turbidite records since 36.6 ka at the Yingqiong continental slope in the northwest of South China Sea[J]. Marine Geology & Quaternary Geology, 2020, 40(5): 15-24. DOI: 10.16562/j.cnki.0256-1492.2019112701

南海西北部莺琼陆坡36.6 ka以来的浊流沉积

基金项目: 国家重点研发计划"ROV精准取样技术应用与南海北部深海沉积过程研究"(2017YFC0306703)
详细信息
    作者简介:

    许莎莎(1993—),女,硕士研究生,地质工程专业,E-mail:1228523269@qq.com

    通讯作者:

    冯秀丽(1962—),女,博士,教授,主要从事海洋沉积与工程环境研究,E-mail:fengxiuli@ouc.edu.cn

  • 中图分类号: P736.4

Turbidite records since 36.6 ka at the Yingqiong continental slope in the northwest of South China Sea

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  • 摘要: 对取自南海西北部莺琼陆坡的ZK3岩心进行了AMS14C测年、沉积物粒度分析、地球化学元素分析等,结合萨哈-兰迪姆相浊流环境判别及C-M图的分析结果,识别了南海西北部莺琼陆坡的浊流沉积,讨论了浊流发育的成因及环境气候变化对南海陆坡沉积环境的影响。研究表明:ZK3岩心主要发育了36.6 kaBP以来的晚更新世和全新世地层,浊流沉积发育,初步识别出7.4~8.3、12.8~13.5、15.5~17.2、18.7~20.7 m这4个特征明显的浊积层,其中有3次浊积事件发生于末次冰期。有利的地形、丰富的物源、活跃的海平面变化及气候变化是触发浊流的主要因素。
    Abstract: The cores of ZK3 collected from the Yingqiong slope in the northwest of South China Sea were dated with AMS14C dating, and analyzed for grain sizes and geochemical elements. The Shakha-Landim method for discrimination of turbidity environment and the C-M diagram for turbidite deposits, are also used to recognize the turbidity sediments. Detailed discussion is devoted to the formation of turbidity current and the impacts of the climate change onto the sedimentary environment. The study shows that sediments of core ZK3 were deposited in the time of Pleistocene and Holocene since 36.6 ka. Four layers of turbidite with obvious features occur in the intervals of 7.4~8.3, 12.8~13.5, 15.5~17.2 and 18.7~20.7 m respectively, corresponding to three turbidity events during the last glacial stage. Favorable topography, abundant material supply, active sea level fluctuation and climate change are the main causes for the origin of the turbidity currents.
  • 图  1   ZK3岩心位置图

    Figure  1.   Location of core ZK3

    图  2   ZK3岩心测年结果和沉积速率变化图

    Figure  2.   Dating results and sedimentation rate of the core ZK3

    图  3   ZK3岩心沉积物类型三角图解

    Figure  3.   Classification of the sediments from core ZK3

    图  4   岩心沉积物组成与粒度参数垂向变化

    Figure  4.   Vertical variation of sediment composition and grain size parameters

    图  5   ZK3岩心的粒度C-M

    Figure  5.   C-M diagram of Core ZK3

    图  6   海平面升降曲线

    Figure  6.   Sea level fluctuation curve

    图  7   ZK3岩心元素比值及碳酸钙含量垂向变化

    Figure  7.   Vertical change in element ratio and calcium carbonate content in core ZK3

    图  8   研究区周边洋流分布图(洋流模式参考文献[40-41])

    Figure  8.   Current distribution around the study area(see reference [40-41] for current model)

    表  1   ZK3岩心沉积物组成与粒度参数

    Table  1   Composition and grain size parameters of the sediments from core ZK3

    粒度参数砂/%粉砂/%黏土/%MdMzσISkIKg
    平均值1.1669.8329.010.0080.0071.6250.1611.016
    最大值3.8574.8033.790.0090.0081.7560.2231.122
    最小值0.0064.2823.780.0060.0061.5250.1000.965
    下载: 导出CSV

    表  2   ZK3岩心各层位萨哈-兰迪姆相浊流环境判别结果

    Table  2   Identification of Turbidity current environment with Sakha-Landim facies diagram for each layer of core ZK3

    层位Y层位Y
    ZK3 S-9-7.405.619ZK3 S-29-16.205.697
    ZK3 S-10-7.705.606ZK3 S-31-17.205.741
    ZK3 S-11-8.305.657ZK3 S-35-18.705.885
    ZK3 S-22-12.805.530ZK3 S-37-19.405.748
    ZK3 S-24-13.505.549ZK3 S-41-20.705.860
    ZK3 S-28-15.505.521
    下载: 导出CSV
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  • 收稿日期:  2019-11-26
  • 修回日期:  2020-01-07
  • 网络出版日期:  2020-10-20
  • 刊出日期:  2020-09-30

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