Abstract
Integration of structural, stratigraphical, and sedimentological data and instrumental records of some recent low-energy seismic events in the Murge area allow us to suggest a new seismotectonic picture of this region, generally considered an aseismic and stable sector of the Apulian foreland.
Keywords
quaternary tectonics;Apulian foreland;Murge region
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DOI: https://doi.org/10.4401/ag-3876
Published by INGV, Istituto Nazionale di Geofisica e Vulcanologia - ISSN: 2037-416X