EVOLUZIONE TETTONICA PLIO-QUATERNARIA DELL'AREA REATINA: IMPLICAZIONI PER POSSIBILI SCENARI DI PERICOLOSITA' DA TERREMOTO

Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1457

Title:	EVOLUZIONE TETTONICA PLIO-QUATERNARIA DELL'AREA REATINA: IMPLICAZIONI PER POSSIBILI SCENARI DI PERICOLOSITA' DA TERREMOTO
Other Titles:	Plio-Quaternary evolution of the Rieti region (Central Italy): implications for seismic hazard assessment
Authors:	MICARELLI, L. TONDI, E. CELLO, G.
Keywords:	Appennino Centrale - Bacini intramontani quaternari - faglie attive - pericolosità sismica Central Apennines - Quaternary intramontane basins - active faults - seismic hazard
Issue Date:	2003
Publisher:	Università di Camerino
Citation:	Studi geologici camerti. Nuova serie, 2003/1, pp.81-102
Abstract:	Structural data acquired along the main structures outcropping in the Rieti region, integrated with stratigrafie and geomorfologica! data, allowed us to define the Plio-Quatemary evolution of the Rieti basin area. During the Middle-Upper Pleistocene, strike-slip tectonics with rigth lateral motion along E-W trending faults and left lateral slip along N-S trending faults, followed a generai extensional regime which, in the Upper Pliocene, originated the Rieti intramontane basin. [...]
URI:	http://193.204.8.201:8080/jspui/handle/1336/834
ISSN:	1827-1979
Appears in Volumess:	Volume 2003/1

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STUDI GEOLOGICI CAMERTI