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The contribution of an urban gravity survey to the determinable perspective of Athens city (Greece) underground structure

机译:城市重力调查对雅典城市(希腊)地下结构的可确定视角的贡献

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An urban gravity survey with more than 1120 measurements was carried out in order to adumbrate the deeper subsurface of Athens city basin. The aim was to gather quantitative information of the subsurface structure derived from the acquisition of gravity measurements. At first, a gravity base network has been established for the data collection. The standard data reduction has been carried out along with an additional Building Correction that has been calculated due to the urban characteristics. Subsequently, the residual anomaly was isolated with the contribution of the Fourier filters. The Euler deconvolution has been applied, with two different techniques, providing depth solutions for the residual maps. Based on these maps, we managed to retrieve quantitative information for the depths of anomalous sources, ranging between 500 and 3760 m. Moreover, unconstrained three-dimensional density models of the area have been constructed in order to obtain a good image of the subsurface, up to depths of 4500 m. For each three-dimensional density model, we provide a couple of images; one illustrating only the structures of lower densities and one other only with the structures of higher densities, in an effort to delineate better the tectonic structures. Finally, two geophysicalgeological profiles (2.75D) have been constructed, along which the geotectonic regime of the subsurface seems to be adumbrated in a better way. Major known tectonic structures of Athens basin have been identified beneath the surface.
机译:进行了超过1120次测量的城市重力调查,以便遵守雅典城市盆地的更深层次的地下。目的是收集来自收购重力测量的地下结构的定量信息。首先,已经为数据收集建立了重力基础网络。已经进行了标准数据减少以及由于城市特征而计算的额外建筑校正。随后,将残留异常与傅立叶滤光器的贡献隔离。应用了欧拉解卷积,具有两种不同的技术,为残余地图提供深度解决方案。基于这些地图,我们设法检索用于异常源深度的定量信息,范围为500至3760米。此外,已经构建了该区域的未经约束的三维密度模型,以获得地下的良好形象,高达4500米的深度。对于每个三维密度模型,我们提供了几张图像;其中仅通过更高密度的结构示出了较小密度的结构,努力拼写构造结构更好。最后,已经建造了两个地球物理学曲线(2.75D),其似乎似乎以更好的方式对地下的地理位置制度似乎是众所周知的。在表面下面已经识别了雅典盆地的主要已知构造结构。

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