Studio gravimatrico della Conca di Sulmona
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Abstract
A gravity survey was carried out to identify the geological and structural features of the Sulmona Basin, an intramontane depression in the central Apennines (eastern Abruzzo). Gravity anomalies have been used for the construction of a 3D model of the area, and gravity data for the construction of Bouguer and residual anomaly maps. These data, together with geological surface data allowed for the understanding of the Plio-quaternary tectonic setting of the basin.
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