In the framework of the Project AGRIFLUID a geoelectrical survey based on the integration of deep and shallow resistivity tomographies has been carried out to better characterise the geological structural setting of the Agri valley (Southern Italy) and in particular to delineate the geometry of the pre-quaternary bedrock. The high valley of the Agri River is a NW-SE trending intermontane basin located in the Southern Apennines an Adriatic-verging fold-andthrust belt mainly derived from the deformation of the African-Apulian passive margin.

Deep Electrical Resistivity Tomographies to Investigate the Pre-Quaternary Bedrock in the Agri High Valley, Southern Italy

E Rizzo;S Piscitelli;
2002

Abstract

In the framework of the Project AGRIFLUID a geoelectrical survey based on the integration of deep and shallow resistivity tomographies has been carried out to better characterise the geological structural setting of the Agri valley (Southern Italy) and in particular to delineate the geometry of the pre-quaternary bedrock. The high valley of the Agri River is a NW-SE trending intermontane basin located in the Southern Apennines an Adriatic-verging fold-andthrust belt mainly derived from the deformation of the African-Apulian passive margin.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/211971
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