Utilizza questo identificativo per citare o creare un link a questo documento: http://dx.doi.org/10.15165/studgeocam-1304
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Campo DCValoreLingua
dc.contributor.authorBIANCA, M.-
dc.contributor.authorCAPUTO, R.-
dc.date.accessioned2017-12-04T09:24:32Z-
dc.date.available2017-12-04T09:24:32Z-
dc.date.issued2004-
dc.identifier.citationStudi geologici camerti, n. speciale, 2004, pp. 33-37it
dc.identifier.issn0392-0631-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/671-
dc.description.abstractIn this paper a detailed morphotectonic analysis of both the Quatemary alluvial and marine terraces of the Agri River (one of the most tectonically active regions of southem Italy) is presented. Here the occurrence of severa! orders of Pleistocene­Holocene fluvial terraces along the whole Agri Valley and the pre­sence of a sequence of Pleistocene-Holocene marine terraces along the Ionian coastal stretch of the river mouth, strongly suggest that the portion of Lucanian Apennines and Bradanic foredeep crossed by the Agri River have undergone a process of tectonic uplifting, ranging from about 0.2 mm/a to more than 2.5 mm/a, during Quatemary.en
dc.publisherUniversità di Camerinoit
dc.subjectAgri River - Active tectonics - Alluvial and marine terracesen
dc.titleA MORPHOTECTONIC ANALYSIS OF THE AGRI VALLEY, SOUTHERN ITALY: ALLUVIAL AND MARINE TERRACES AS INDICATORS OF ACTIVE TECTONICSen
dc.description.pages33-37-
E' visualizzato nelle collezioni:2004: Proceeding of the workshop COST-ACTION 625 "Active fault: analysis processes and monitoring", Camerino, Italy, May 3-6 2002

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