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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1021

Authors: Piccinini, D.*
Cattaneo, M.*
Chiarabba, C.*
Chiaraluce, L.*
De Martin, M.*
Di Bona, M.*
Moretti, M.*
Selvaggi, G.*
Augliera, P.*
Spallarossa, D.*
Ferretti, G.*
Michelini, A.*
Govoni, A.*
Di Bartolomeo, P.*
Romanelli, M.*
Fabbri, J.*
Title: A microseismic study in a low seismicity area of Italy: the Città di Castello 2000-2001 experiment
Issue Date: 2003
Series/Report no.: 46 (6)
URI: http://hdl.handle.net/2122/1021
Keywords: microseismicity
low-angle normalfault
seismic gap
seismic hazard
Abstract: Recent seismological studies contribute to better understand the first order characteristics of earthquake occurrence in Italy, identifying the potential sites for moderate to large size earthquakes. Ad hoc passive seismic experiments performed in these areas provide information to focus on the location and geometry of the active faults more closely. This information is relevant for assessing seismic hazard and for accurately constraining possible ground shaking scenarios. The area around the Città di Castello Basin, in the Northern Apennines (Central Italy), is characterized by the absence of instrumental seismicity (M > 2.5), it is adjacent to faults ruptured by recent and historical earthquakes. To better understand the tectonics of the area, we installed a dense network of seismic stations equipped with broadband and short period seismometers collecting data continuously for 8 months (October 2000-May 2001). The processing of ~ 900 Gbyte of data revealed a consistent background seismicity consisting of very low magnitude earthquakes (ML < 3.2). Preliminary locations of about 2200 local earthquakes show that the area can be divided into two regions with different seismic behaviour: an area to the NW, in between Sansepolcro and Città di Castello, where seismicity is not present. An area toward the SE, in between Città di Castello, Umbertide and Gubbio, where we detected a high microseismicity activity. These findings suggest a probable different mechanical behaviour of the two regions. In the latter area, the seismicity is confined between 0 and 8 km of depth revealing a rather well defined east-dipping, low angle fault 35 km wide that cuts through the entire upper crust down to 12-15 km depth. Beside an apparent structural complexity, fault plane solutions of background seismicity reveal a homogeneous pattern of deformation with a clear NE-SW extension.
Appears in Collections:Manuscripts
04.06.10. Instruments and techniques
04.06.06. Surveys, measurements, and monitoring
Annals of Geophysics

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