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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2002 Vol. Speciale p.61.pdf | 594,1 kB | Adobe PDF | View/Open |
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