Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1362
Title: COMPARISON BETWEEN GEOLOGICAL AND MORPHOMETRIC DATA IN THE PERIADRIATIC BASIN (CENTRAL ITALY)
Authors: CURRADO, C.
D'AMBROGI, C.
Keywords: Neotectonic - Morphometric Parameters - Periadriatic Basin - Drainage network
Neotettonica - Parametri morfometrici - Bacino periadriatico - Reticolo idrografico
Issue Date: 2002
Publisher: Università di Camerino
Citation: Studi geologici camerti, n. speciale, 2002, pp. 61-67
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. [...]
URI: http://193.204.8.201:8080/jspui/handle/1336/737
ISSN: 0392-0631
Appears in Volumess:2002: International workshop "Large-scale vertical movements and related gravitational processes", Camerino-Roma 21th-26th June, 1999, Proceedings

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