1. Studi Geologici Camerti
  2. 2 - Studi Geologici Camerti - Volume Speciale
  3. 2002: International workshop "Large-scale vertical movements and related gravitational processes", Camerino-Roma 21th-26th June, 1999, Proceedings
Utilizza questo identificativo per citare o creare un link a questo documento: http://dx.doi.org/10.15165/studgeocam-1369
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Campo DCValoreLingua
dc.contributor.authorMOLIN, P.-
dc.contributor.authorDRAMIS, F.-
dc.contributor.authorLUPIA PALMIERI, E.-
dc.date.accessioned2017-12-07T09:50:03Z-
dc.date.available2017-12-07T09:50:03Z-
dc.date.issued2002-
dc.identifier.citationStudi geologici camerti, n. speciale, 2002, pp. 135-145it
dc.identifier.issn0392-0631-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/743-
dc.description.abstractA model of the Plio-Pleistocene evolution of the northem Calabria Peri-ionian sector, between Corigliano and Capo Trionto, is proposed on the basis of morphological and sedimentary analy­sis. The main morphological features are gently undulated surfaces on the Sila Massif summits, five orders of fluvial terraces (Qt1, Qt2, Qt3, Qt4, and Qt5) located in the watersheds of the hilly coastal belt, and structural scarps of a NW-SE trending extensional fault system, which separates the Sila Massif from the hilly coastal belt. [...]en
dc.publisherUniversità di Camerinoit
dc.subjectuplift - Northem Calabria - fan-delta - climatic changes - Plio-Pleistoceneen
dc.subjectsollevamento - Calabria settentrionale - delta-conoidi - variazioni climatiche - Plio-Pleistoceneit
dc.titleTHE PLIOCENE-QUATERNARY UPLIFT OF THE IONIAN NORTHERN CALABRIA COASTAL BELT BETWEEN CORIGLIANO CALABRO AND CAPO TRIONTOen
dc.description.pages135-145-
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