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Peculiar Morphologies of Subaqueous Landslide Deposits and Their Relationship to Flow Dynamics

机译:岩石滑坡沉积物的特殊形态及其与流动动态的关系

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The morphology of subaqueous landslide deposits is seldom analyzed quantitatively or at least semi-quantitatively with regard to the dynamics of the flow. However, the peculiar morphology of the deposits can reveal information on the mechanics of propagation of the mass movement and on the mechanism of emplacement. Horseshoe-shaped deposits and oriented blocks are two peculiar morphologies of subaqueous landslide which have been identified in this paper. Both morphologies have been described in a qualitative way by considering the shape of the deposit and the geomorphological features of the areas of emplacement. Furthermore, these morphologies have been analyzed in a quantitative way by means of mathematical and numerical approaches. The close relationship between these morphologies and the landslide mechanism of propagation and emplacement has been thus preliminary demonstrated by accounting for the interaction between moving mass and the ambient fluid.
机译:关于流动的动态,可以定量地或至少半定量分析水分垫层沉积物的形态。然而,沉积物的特殊形态可以揭示关于批量移动传播的机制和施加机制的信息。马蹄形沉积物和导向块是本文已识别的亚水底滑坡的两个特殊形态。通过考虑沉积物的形状和施加区域的地貌特征,已经以定性方式描述了两种形态。此外,通过数学和数值方法以定量方式分析了这些形态。因此,通过算用于移动质量与环境流体之间的相互作用,已经初步证明了这些形态与播种机制的密切关系。

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