Utilizza questo identificativo per citare o creare un link a questo documento: http://dx.doi.org/10.15165/studgeocam-1449
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dc.contributor.authorMUTO, F.-
dc.contributor.authorROBUSTELLI, G.-
dc.contributor.authorSCARCIGLIA, F.-
dc.contributor.authorSPINA, V.-
dc.date.accessioned2018-01-17T09:27:21Z-
dc.date.available2018-01-17T09:27:21Z-
dc.date.issued2002-
dc.identifier.citationStudi geologici camerti. Nuova serie, 2002/1, pp.135-145it
dc.identifier.issn1827-1979-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/826-
dc.description.abstractThe Late Quatemary evolution of the western Coastal Range, an area of northem Calabria located along the Tyrrhenian coast, has been reconstructed by means of integrated stratigraphical and geomorphological studies. We have focused on alluvial-fan landforms and deposits. Three generations of alluvial-fans (Middle?-Upper Pleistocene to Holocene), telescopically arranged, have been distinguished, also on the basis of facies analysis, which has indicated that gravity processes were dominant in fan construc­tion; in particular debris-avalanche, debris-flow and sheetflood deposits have been characterised. [...]it
dc.publisherUniversità di Camerinoit
dc.subjectAlluvial fans - facies analysis - sea-level changes - Late Quaternary - Tyrrhenian Sea - Southem Italyit
dc.subjectConoidi alluvionali - analisi di facies - varia­zioni del livello del mare - Tardo Quaternario - Mar Tirreno - Italia Meridionaleit
dc.titleLATE QUATERNARY FAN DEVELOPMENT AND SEA-LEVEL CHANGES ALONG THE TYRRHENIAN COAST OF CALABRIA (SOUTHERN ITALY).en
dc.title.alternativeVariazioni del livello del mare e sviluppo di sistemi di conoide tardo-quaternari lungo la costa tirrenica della Calabria (Italia Meridionale)it
dc.description.pages135-145-
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