Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1201
Title: IL PLIO-PLEISTOCENE NELL'AREA MEDIO-ALTA DEL BACINO DEL F. TEVERE: POSSIBILE MODELLO MORFOTETTONICO
Authors: CATTUTO, C.
CENCETTI, C.
GREGORI, L.
Keywords: Geomorfologia - Neotettonica - Idrogra­fia - Quaternario - Umbria
Geomorphology - Neotectonics - Idrography - Quaternary - Umbria (Italy)
Issue Date: 1992
Publisher: Università di Camerino
Citation: Studi geologici camerti, n. speciale, 1992, pp. 103-108 + carta + err.corr. carta
Abstract: By means of morphotectonic and paleogeographic data relative to the western side of Umbria-Marche Apennine (Cen­tra! Italy), the Authors describe a simple tectonic model for the paleogeographic evolution of this area during Pliocene and Pleistocene. The rising of the Centrai Apennine during the Ac­quatraversa phase marks the regression of the pliocenic sea in the western side of the chain and produces the formation or the deepening of the "intermountain basins".
URI: http://193.204.8.201:8080/jspui/handle/1336/555
ISSN: 0392-0631
Appears in Volumess:1992/1: "Evoluzione geomorfologica e tettonica quaternaria dell'Appennino centro-meridionale"



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