TETTONICA E SEDIMENTAZIONE (LIAS-PLEISTOCENE) NELLA MEDIA VALLE DEL SALTO  (RIETI - ITALIA CENTRALE)

Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1440

Title:	TETTONICA E SEDIMENTAZIONE (LIAS-PLEISTOCENE) NELLA MEDIA VALLE DEL SALTO (RIETI - ITALIA CENTRALE)
Other Titles:	Tectonics and sedimentation (Lias-Pleistocene) in the middle Salto valley (Rieti, central Italy
Authors:	CENTAMORE, E. NISIO, S.
Keywords:	Lazio nord-orientale - Valle del Salto - Tettonica sinsedimentaria - compressione neogenica - Sollevamento quaternario - Tettonica estensionale North-eastern Latium - Salto River Valley - Syn-sedimentary tectonics - Neogenic compression - Quaternary uplift - Extensional tectonics
Issue Date:	2002
Publisher:	Università di Camerino
Citation:	Studi geologici camerti. Nuova serie, 2002/1, pp.53-70 + 1 carta
Abstract:	The middle Salto River Valley is a key area to understand the geologica! evolution of Centrai Italy. The study area lies near the convergence zone between the pelagic Umbrian-MarcheanSabine domain and the neritic Latium-Abruzzi domain, where a Middle Lias master fault formed and along which the AnconaAnzio line developed. Two main structural elements, the OlevanoAntrodoco line and the Fiamignano-Micciani fault, divide the area into three sectors, each with its own evolutionary trend and structural style. From west to east they are: the Navegna Unit, the Salto Unit and the Nuria Unit. [...]
URI:	http://193.204.8.201:8080/jspui/handle/1336/818
ISSN:	1827-1979
Appears in Volumess:	Volume 2002/2

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STUDI GEOLOGICI CAMERTI