GIS analysis operations are applied to both a set of available vertical electric sounding data (VES), and topographical data using digital elevation models (DEM) allowing the reconstruction of the approximate three-dimensional shape of the Cubeta del Saltador basin-floor and its limiting faults, as well as affording the thickness of the Plio-Quaternary sedimentary filling. From the morphological configuration of the basin floor, several furrows related to Plio-Quaternary fluvial systems are identified.
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