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Rock Mass Characterization Coupled with Seismic Noise Measurements to Analyze the Unstable Cliff Slope of the Selmun Promontory (Malta)

机译:岩体表征与地震噪声测量相结合,分析塞尔蒙海角(马耳他)的不稳定峭壁坡度

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摘要

In the Mediterranean area, cliff slopes represent widespread high-risk landforms as they are highly frequented touristic places often interested by landslide processes. Malta represents a significant case study as several cliffs located all around the island are involved in instability processes, as evidenced by wide block-size talus distributed all along the coast line. These diffused instabilities are related to the predisponding geological setting of Malta Island, i.e. the over-position of grained limestone on plastic clay deposits, that induces lateral spreading phenomena associated to falls and topples of different-size rock blocks and is responsible for a typical landscape with stable plateau of stiff rocks bordered by unstable cliff slopes. The ruins of Gƫajn ƪadid Tower, the first of the thirteen watchtowers built in 1658 by the Gran Master Martin de Redin, stand out in the Selmun area. Currently the safety of this important heritage site, already damaged by an earthquake on October 12th 1856, is threaten by a progressive moving of the landslide process towards the stable plateau area. During autumn 2015, a field campaign was realized to characterize the jointed rock mass. A detailed engineering-geological survey was carried out to reconstruct the geological setting and to define the mechanical properties of the rock mass. Based on the surveyed joint spatial distribution, 58 single-station noise measurements were deployed to cover both the unstable zone and the stable area. The obtained 1-hour records were analyzed in the frequency domain for associating vibrational evidences to different instability levels, i.e. deriving the presence of already isolated blocks by the local seismic response. The here presented results can be a useful contribute to begin to asses defense strategies for the Selmun Promontory, in the frame of managing the landslide risk in the study area and preserving the local historical heritage.
机译:在地中海地区,悬崖斜坡代表着广泛的高风险地貌,因为它们是经常被滑坡过程所吸引的频繁旅游的地方。马耳他是一个重要的案例研究,因为遍布岛上的几处悬崖都参与了不稳定过程,沿海岸线分布的宽块状距骨证明了这一点。这些扩散的不稳定性与马耳他岛的地质环境有关,即,在塑料粘土沉积物上的粒状石灰岩位置过大,引起与不同大小的岩石块的倒塌和倾倒有关的横向扩展现象,并构成了典型的景观。具有稳定的高原岩石和不稳定的悬崖斜坡。古尔·马丁·雷丁(Grand Master Martin de Redin)于1658年建造的十三座watch望塔中的第一座,古尚·阿迪德塔(GajnƪadidTower)的废墟在塞尔蒙地区十分突出。目前,这个重要的遗产地的安全已经受到1856年10月12日地震的破坏,但由于滑坡过程逐渐向稳定的高原地区转移而受到威胁。在2015年秋天,一场野外运动得以实现,以表征节理岩体。进行了详细的工程地质勘测,以重建地质环境并定义岩体的力学特性。根据调查的联合空间分布,部署了58个单站噪声测量值,覆盖了不稳定区域和稳定区域。在频域中对获得的1小时记录进行分析,以将振动证据与不同的不稳定性级别相关联,即通过本地地震响应得出已经隔离的块的存在。在管理研究区域的滑坡风险和保存当地历史遗产的框架下,此处介绍的结果可能有助于开始评估塞尔蒙海角的防御策略。

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