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Contourite and mixed turbidite-contourite systems in the Mozambique Channel (SW Indian Ocean): Link between geometry, sediment characteristics and modelled bottom currents

机译:莫桑比克频道(SW印度洋)中的轮廓座和混合浊磁石 - 连续石系统:几何,沉积物特性和建模底流之间的联系

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摘要

Oceanic currents can profoundly reshape the seafloor and even modify the characteristics of turbidite systems. Multiple ero-sional and depositional features directly formed by bottom currents (i.e. contourites), as well as by the interaction between bottom currents and turbidity currents or turbidite systems (i.e. mixed turbidite-contourite systems) have been identified in the Mozambique Channel (SW Indian Ocean) in multibeam bathymetry, seismic reflection data, sub-bottom profiler images and sediment cores. In this study, we characterise the morphology, stacking pattern and sedimentary characteristics of these sedimentary systems, and analysed the properties of bottom currents at these systems using a hydrodynamic numerical model. Modelled bottom currents are the highest at abraded surfaces and moats, but they also display a relatively high variability, suggesting that the observed erosion is not the result of a constant or persistent current but rather of episodes of intense circulation. Modelled bottom currents at contourite terraces are not significantly different from currents at related plastered drifts, where accumulation is enhanced. The formation of contourite terraces can thus not solely be explained by the mean oceanic circulation and eddies, implying that other processes such as internal waves may play a relevant role in their formation. Three different types of mixed turbidite-contourite systems were observed: one characterised by asymmetric channel-levee systems formed by the synchronous interaction of bottom currents and turbidity currents, one characterised by a phased interaction that resulted in the erosion of the channel flanks by bottom currents, and another one in which both synchronous and phased interaction played a relevant role in the evolution of the system. Finally, we propose a simplified classification of contourites that can be applied to any contourite system worldwide, and that comprises erosional and depositional features, including muddy and sandy contourite deposits.
机译:海洋电流可以深刻地重塑海底,甚至改变浊度系统的特点。通过底部电流直接形成的多个Ero-anional和沉积特征,以及莫桑比克通道(SW印度人海洋)在多次浴浴,地震反射数据,次底分布器图像和沉积物核心。在该研究中,我们表征了这些沉积系统的形态,堆叠模式和沉积特征,并使用流体动力学数值模型分析了这些系统的底部电流的性质。建模的底部电流是磨损表面和毛的最高电流,但它们也显示出相对高的变化性,表明观察到的侵蚀不是恒定或持续的电流的结果,而是强烈循环的剧集。在Contulite露台上的建模底部电流与相关涂抹漂移的电流没有显着不同,其中累积增强。因此,不仅可以由平均海洋循环和漩涡解释的轮廓化露台的形成,这意味着诸如内波等其他过程可能在其形成中发挥相关作用。观察到三种不同类型的混合浊磁石 - 连续石系统:一种特征在于由底部电流的同步相互作用形成的不对称通道 - 堤坝系统,其特征在于通过底部电流产生沟道侧面的相互作用的相互作用。并且另一个同步和相互作用的另一个在系统的演变中起着相关的作用。最后,我们提出了一种可以应用于全球任何轮廓技术系统的轮廓技术的简化分类,并且包括侵蚀和沉积特征,包括泥泞和含有含有泥质的砂质矿床。

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  • 来源
    《Oceanographic Literature Review》 |2021年第6期|1260-1260|共1页
  • 作者单位

    Faculty of Geosciences University of Bremen Bremen 28359 Germany;

    Faculty of Geosciences University of Bremen Bremen 28359 Germany;

    Faculty of Geosciences University of Bremen Bremen 28359 Germany;

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