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Integrated use of well and geophysical data for constructing 3D geological models in shallow aquifers: a case study at the Tymbakion basin, Crete, Greece

机译:综合使用井和地球物理数据,用于构建浅含水层3D地质模型 - 以TYMBAKION盆地,克里特岛,希腊为例

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摘要

3D geological models increase our understanding of the subsurface structures and the spatial distribution of sediment's properties. The models can be applied in different aspects of geology and assist in reaching to more robust conclusions. In this study, a methodology for constructing a 3D geological model of the Tymbakion basin, Crete, Greece, is presented. The model is based on a dense array of newly acquired Transient Electromagnetics measurements (TEM), legacy Vertical Electrical Soundings (VES), and well data that cover an area of approximately 35 km(2) and 500 m in depth. The model is representative of the Plio-Quaternary section, which hosts the Tymbakion shallow aquifer. The study area is one of the main agricultural sites of Greece with touristic activity. The model reveals the existence of 12 faults, which are not observed on the surface, and provides the lithological and resistivity distribution on the subsurface. The importance of the model relies in the fact that it gives a better insight into the hydrogeological setting of the shallow aquifer and the problems related to the intensive water exploitation during the last decades.
机译:3D地质模型增加了我们对地下结构的理解和沉积物的空间分布。该模型可应用于地质的不同方面,并协助达到更强大的结论。在这项研究中,提出了一种构建Tymbakion盆地,克里特岛,希腊的3D地质模型的方法。该模型基于致密的新获得的瞬态电磁测量(TEM),传统垂直电探测(VES),以及井数据,覆盖大约35公里(2)和500米的深度。该模型代表了托管Tymbakion浅含水层的Plio - 四元部分。研究区是希腊的主要农业遗址之一,具有旅游活动。该模型显示出12个故障的存在,在表面上未观察到,并在地下提供岩性和电阻率分布。该模型的重要性依赖于它还能够更好地了解浅层含水层的水文地质环境以及过去几十年中与强化水剥削相关的问题。

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