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Morphological, stratigraphical and structural investigations integrated with palaeomagnetic and tephrostratigraphic studies and 40 Ar/ 39 Ar measurements allowed us to define the Quaternary tectonic–sedimentary evolution of the epicentral area of the L'Aquila 2009 earthquake (M w 6.3). This area roughly matches the Paganica–San Demetrio–Castelnuovo (PSC) intermountain basin...
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