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Regional Hazard Assessment of Earthquake-Triggered Slope Instabilities Considering Site Effects and Seismic Scenarios in Lorca Basin (Spain)

机译:考虑地点效应和地震情景的洛尔卡盆地地震触发斜坡不稳定性的区域危险性评估(西班牙)

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摘要

We present a regional hazard assessment of earthquake-triggered slope instabilities based on specific seismic scenarios and taking into account soil and topographic amplification effects. We followed Newmark’s sliding rigid-block methodology implemented in a geographic information system (GIS) with the aim of producing regional maps in terms of critical acceleration and Newmark displacements for selected seismic scenarios. Strong ground-motion amplification site effects have been considered, particularly the topographic factor, by means of designing a GIS tool based on terrain geometry features and Eurocode-8 provisions. Three different concepts of seismic scenarios are considered in this work: probabilistic, pseudo-probabilistic, and deterministic. The study area is the Lorca Basin, located in the Eastern Betic Cordillera, one of the most seismically active regions of southeast Spain. The obtained Newmark displacement maps are compared to the distribution of known slope instabilities in the area. Future seismically induced slope instabilities in the Lorca Basin appear to be limited to isolated rock slides and rockfalls. Only the deterministic scenario (M_w > 6.7) seems capable of producing widespread slope instabilities, mainly rock slides, rockfalls, and landslides.
机译:我们基于特定的地震场景并考虑了土壤和地形的放大效应,提出了地震触发的边坡不稳定性的区域危险性评估。我们遵循在地理信息系统(GIS)中实施的纽马克滑动刚性块方法,目的是针对特定地震场景,根据临界加速度和纽马克位移生成区域地图。通过设计基于地形几何特征和Eurocode-8规定的GIS工具,已经考虑到强烈的地面运动放大效应,特别是地形因素。在这项工作中考虑了三种不同的地震情境概念:概率论,伪概率论和确定论。研究区域是洛卡盆地,它位于东部比蒂科迪勒拉(Betic Cordillera),是西班牙东南部地震最活跃的地区之一。将获得的Newmark位移图与该地区已知坡度不稳定性的分布进行比较。洛尔卡盆地未来的地震诱发的斜坡失稳似乎仅限于孤立的岩石滑坡和崩塌。只有确定性方案(M_w> 6.7)似乎能够产生广泛的边坡失稳,主要是岩石滑坡,崩塌和滑坡。

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