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Near-surface Voids in the Neapolitan Volcanic Tuff (Italy) Detected by Seismic Refraction Tomography

机译:由地震折射断层扫描检测到的Neakitan火山凝灰岩(意大利)中的近表面空隙

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The Neapolitan area (Italy) is affected by the presence of shallow man-made cavities in volcanic tuffs that were used in the past as building material. Therefore, the identification of these voids is a fundamental prerequisite for the minimization of subsurface collapse risks. In the past few years, several authors have shown that the geophysics prospecting methods can provide a most convenient solution to detecting underground voids. In this work we show how the seismic refraction tomography represents a powerful tool for the detection of near-surface tuff-cavities located in Casamarciano, Naples. The interpolation of the velocity models, allowed us to build a three-dimensional model of the tuff basement top and to show the lateral extend of the voids. The cavity location detected by seismic refraction tomography has been subsequently confirmed by four core-drilling made in the area.
机译:Neapolitan地区(意大利)受到过去作为建筑材料中使用的火山凝灰岩中存在浅人造空腔的影响。因此,这些空隙的鉴定是最小化地下崩溃风险的基本先决条件。在过去的几年里,几位作者表明,地球物理勘探方法可以为检测地下空隙提供最方便的解决方案。在这项工作中,我们展示了地震折射断层造影如何代表检测位于Casamarciano,那不勒斯的近表面凝灰岩的强大工具。速度模型的插值使我们能够构建牙龈基底顶部的三维模型,并显示空隙的横向延伸。随后通过在该地区制造的四个芯钻​​孔来证实由地震折射断层扫描断层扫描的腔位置。

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