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Mapping basin-wide subaquatic slope failure susceptibility as a tool to assess regional seismic and tsunami hazards

机译:绘制全盆地亚水底斜坡破坏敏感性图,作为评估区域地震和海啸危害的工具

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This study of subaquatic slope failures in Lake Lucerne, central Switzerland, presents a new concept for evaluating basin-wide slope stability through time as a potential tool for regional seismic and tsunami hazard assessments. Previously acquired high-resolution bathymetry and reflection seismic data, as well as sedimentological and in situ geotechnical data, provide a comprehensive data base to use this lake as a ‘‘model basin’’ to investigate subaquatic landslides and related geohazards. Available data are implemented into a basin-wide slope model. In a Geographic Information System (GIS)-framework, a pseudo-static limit equilibrium infinite slope stability equation is solved for each model point representing reconstructed slope conditions at different times in the past, during which earthquake-triggered landslides occurred. Comparison of reconstructed critical stability conditions with the known distribution of landslide deposits reveals minimum and maximum threshold conditions for slopes that failed or remained stable, respectively. The resulting correlations reveal good agreements and suggest that the slope stability model generally succeeds in reproducing past events. The basin-wide mapping of subaquatic slope failure susceptibility through time thus can also be considered as a promising paleoseismologic tool. Furthermore, it can be used to assess the present-day slope failure susceptibility, allowing for identification of location and estimation of size of future, potentially tsunamigenic subaquatic landslides.
机译:这项对瑞士中部卢塞恩湖的亚水底斜坡破坏的研究提出了一种新的概念,即通过时间评估流域范围内的斜坡稳定性,可以作为评估区域地震和海啸危险的潜在工具。以前获得的高分辨率测深和反射地震数据,以及沉积学和原位岩土数据,提供了一个综合的数据库,可将该湖用作研究水下水滑坡和相关地质灾害的“模型盆地”。现有数据被实现为流域范围内的坡度模型。在地理信息系统(GIS)框架中,针对代表过去不同时间重建的斜坡条件的每个模型点,求解了一个拟静力极限平衡无限边坡稳定性方程,在此期间发生了由地震触发的滑坡。将重建的临界稳定条件与滑坡沉积物的已知分布进行比较,可以发现分别失败或保持稳定的边坡的最小和最大阈值条件。由此产生的相关性揭示了良好的一致性,并表明边坡稳定性模型通常可以成功地再现过去的事件。因此,整个盆地的水底亚坡失稳敏感性随时间变化的映射也可以被认为是有前途的古地震学工具。此外,它可用于评估当今的边坡破坏敏感性,从而可以确定位置并估计未来可能发生海啸的亚水生滑坡的大小。

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