COMPARISON BETWEEN GEOLOGICAL AND MORPHOMETRIC DATA IN THE PERIADRIATIC BASIN (CENTRAL ITALY)

Utilizza questo identificativo per citare o creare un link a questo documento: http://dx.doi.org/10.15165/studgeocam-1362

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Campo DC	Valore	Lingua
dc.contributor.author	CURRADO, C.	-
dc.contributor.author	D'AMBROGI, C.	-
dc.date.accessioned	2017-12-07T08:47:02Z	-
dc.date.available	2017-12-07T08:47:02Z	-
dc.date.issued	2002	-
dc.identifier.citation	Studi geologici camerti, n. speciale, 2002, pp. 61-67	it
dc.identifier.issn	0392-0631	-
dc.identifier.uri	http://193.204.8.201:8080/jspui/handle/1336/737	-
dc.description.abstract	The existing morphotectonic setting of the Periadriatic Basin results not only from the interactions between syn-sedimentary tectonics, climatic changes and eustatism, but also from a generalized uplifting process. In particular, during the Plio-Pleistocene time, the activity of severa! transversal fault systems (N20°-35°E, N45°-60°E), corresponding to pre-existing tectonic elements cutting the pre-Pliocene basement, has given rise to the subdivision of the area into severa! sectors cha:racterized by differential vertical movements. [...]	en
dc.publisher	Università di Camerino	it
dc.subject	Neotectonic - Morphometric Parameters - Periadriatic Basin - Drainage network	en
dc.subject	Neotettonica - Parametri morfometrici - Bacino periadriatico - Reticolo idrografico	it
dc.title	COMPARISON BETWEEN GEOLOGICAL AND MORPHOMETRIC DATA IN THE PERIADRIATIC BASIN (CENTRAL ITALY)	en
dc.description.pages	61-67	-
E' visualizzato nelle collezioni:	2002: International workshop "Large-scale vertical movements and related gravitational processes", Camerino-Roma 21th-26th June, 1999, Proceedings

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STUDI GEOLOGICI CAMERTI