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Joint interpretation of seismic refraction tomography and electrical resistivity tomography by cluster analysis to detect buried cavities

机译:射击折射断层扫描和电阻率断层扫描的联合解释群体分析检测埋空腔

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In the last few years, the geophysical methods of seismic refraction tomography (SRT) and electrical resistivity tomography (ERT) are among the most used geophysical techniques for the reconstruction of subsoil geometries, for the investigation of underground cavities and also for the archaeological prospecting. However, the main disadvantage of each geophysical method is the difficulty of final interpretation of the data In order to eliminate artifacts and generally improve the reliability and accuracy of geophysical interpretation, it is useful to perform a joint approach of different geophysical methods, also introducing the a priori information. In this work, it is shown the integrated study of seismic refraction tomography and electrical resistivity tomography techniques, the two geophysical methods are tested on both synthetic and real data and the integration of data is useful in detecting buried cavities and also evaluate their geometric characteristics. Likelihood parameters has been defined and tested, in order to help recognizing voids from other lithological structures. Finally, a statistical approach based on duster analysis of the P-wave velocity, the density of the seismic rays and the electrical resistivity of the synthetic and experimental models was used. Multi-space duster distribution maps were built, allowing to better define and interpret the anomalies of the subsoil. (C) 2020 Elsevier B.V. All rights reserved.
机译:在过去的几年中,地震折射断层扫描(SRT)和电阻率断层扫描(ERT)的地球物理方法是用于改变底体几何形状的最常用的地球物理技术,用于对地下腔和考古勘探的调查。然而,每个地球物理方法的主要缺点是难以释放数据的难度,以消除伪影,一般提高地球物理解释的可靠性和准确性,执行不同地球物理方法的联合方法是有用的,也有助于介绍先验信息。在这项工作中,示出了对地震折射断层扫描和电阻率断层扫描技术的综合研究,在合成和实际数据上测试了两个地球物理方法,并且数据的集成在检测埋藏空腔并评估其几何特征。似然参数已被定义和测试,以帮助识别来自其​​他岩性结构的空隙。最后,使用了一种基于粉波速度分析的统计方法,使用了地震光线的密度和合成和实验模型的电阻率。构建了多空间除尘器分发图,允许更好地定义和解释子系统的异常。 (c)2020 Elsevier B.V.保留所有权利。

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