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High-resolution acoustic data revealing periplatform sedimentary characteristics in the Xisha Archipelago, South China Sea

机译:高分辨率声学数据揭示南海西沙群岛的Periplatform沉积特征

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摘要

Newly collected high-resolution acoustic data are used to describe the morphologies and sedimentary characteristics along the slopes of isolated carbonate platforms in the Xisha (Paracel) Archipelago. Based on multibeam bathymetric and seismic data, we have identified seven types of morphological and depositional features around the platforms, including erosive grooves, mass transport deposits, gullies, confined channels, canyons, mounded sediments, and marginal contourite depressions. The occurrence of erosive channelized features around the platforms indicates that gravity flow is a major sediment-export mechanism for the transportation of excess neritic carbonates towards the slope. Marginal contourite depressions and mounded sediments are interpreted as bottom-current reworking products, suggesting an important role of bottom current and deepwater circulation of the South China Sea in shaping the slope morphology of the carbonate platforms. Furthermore, the bottom-current products tend to develop along the slopes of the carbonate platforms at the Xisha Uplift margin; in particular, erosional features formed by bottom current frequently occur in the southern side of the carbonate platforms. By comprehensive analysis of morphological and depositional features, we establish a facies model around the carbonate platforms to interpret different sedimentary transport processes, such as off-platform and along-slope sediment transport processes. These findings highlight a notable and complex relay-style channelized transport system consisting of grooves/gullies-channels-canyons, which has implications for linking neritic carbonate platforms into deep-sea basins.
机译:新收集的高分辨率声学数据用于描述沿XISHA(帕拉凯尔)群岛的孤立碳酸盐平台斜坡的形态和沉积特征。基于多孔碱基和地震数据,我们已经确定了七种类型的平台上的形态和沉积特征,包括腐蚀槽,大规模运输沉积物,沟渠,限制通道,峡谷,束缚的沉积物和边缘轮廓座凹陷。平台周围的侵蚀通道特征的发生表明重力流动是用于运输过量的碳酸盐朝向坡度的主要沉积物出口机制。边缘轮廓岩抑郁和丘陵沉积物被解释为底部电流的重新加工产品,这表明南海底部电流和深水循环的重要作用在塑造碳酸盐平台的坡度形态方面。此外,底流产品倾向于沿着西沙隆起边缘的碳酸盐平台的斜坡发展;特别地,由底部电流形成的侵蚀特征经常发生在碳酸盐平台的南侧。通过全面分析形态和沉积特征,我们在碳酸盐平台周围建立一个相模型,以解释不同的沉积输送过程,例如离坡平台和斜坡沉积物传输过程。这些发现突出了由凹槽/沟渠通道 - 峡谷组成的值得注意的和复杂的继电器式通道化传输系统,这具有将编织碳酸盐平台连接到深海盆地中的影响。

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  • 来源
    《Oceanographic Literature Review》 |2021年第7期|1485-1485|共1页
  • 作者

    B. Ma; Z. Qin; S. Wu;

  • 作者单位

    Harbin Engineering University Acoustic Science and Technology Laboratory Harbin 150001 China;

    Harbin Engineering University Acoustic Science and Technology Laboratory Harbin 150001 China;

    Harbin Engineering University Acoustic Science and Technology Laboratory Harbin 150001 China;

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  • 正文语种 eng
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