The Subequana valley is one of the easternmost depression of the central Apennines. It is located south of the L’Aquila and Fossa-San Demetrio basins. The formation and evolution of the Subequana valley has been conditioned by the activity of a 8-10- km long, NW-SE trending and SW dipping normal fault system that affects the SW slopes of Mt. Urano which bounds the depression to NE. The fault system, characterised by a complex structural evolution, has been responsible for the displacement of continental deposits spanning the whole Quaternary (MICCADEI et alii, 1997).
Holocene activity of the Subequana Valley-Middle Aterno Valley normal fault system, south of the 2009 L'Aquila earthquake epicentre. Implications for seismic hazard in central Apennines / Falcucci, Emanuela; Gori, Stefano; Moro, Marco; Saroli, Michele; Fubelli, Giandomenico; Galadini, Fabrizio; Fredi, Paola. - In: RENDICONTI ONLINE DELLA SOCIETÀ GEOLOGICA ITALIANA. - ISSN 2035-8008. - ELETTRONICO. - 11:1(2010), pp. 16-17.
Holocene activity of the Subequana Valley-Middle Aterno Valley normal fault system, south of the 2009 L'Aquila earthquake epicentre. Implications for seismic hazard in central Apennines
Saroli, Michele;Fredi, Paola
2010
Abstract
The Subequana valley is one of the easternmost depression of the central Apennines. It is located south of the L’Aquila and Fossa-San Demetrio basins. The formation and evolution of the Subequana valley has been conditioned by the activity of a 8-10- km long, NW-SE trending and SW dipping normal fault system that affects the SW slopes of Mt. Urano which bounds the depression to NE. The fault system, characterised by a complex structural evolution, has been responsible for the displacement of continental deposits spanning the whole Quaternary (MICCADEI et alii, 1997).File | Dimensione | Formato | |
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