Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3448
AuthorsChiaraluce, L.* 
Ellsworth, W.* 
Chiarabba, C.* 
Cocco, M.* 
TitleImaging the complexity of an active normal fault system: The 1997 Colfiorito (central Italy) case study
Issue Date6-Jun-2003
Series/Report no.B6/108 (2003)
DOI10.1029/2002JB002166
URIhttp://hdl.handle.net/2122/3448
KeywordsNormal faulting
double-difference
Umbria-Marche
corss-correlation
relative location
Subject Classification05. General::05.02. Data dissemination::05.02.02. Seismological data 
AbstractSix moderate magnitude earthquakes (5 < Mw < 6) ruptured normal fault segments of the southern sector of the North Apennine belt (central Italy) in the 1997 Colfiorito earthquake sequence. We study the progressive activation of adjacent and nearby parallel faults of this complex normal fault system using1650 earthquake locations obtained by applying a double-difference location method, using travel time picks and waveform cross-correlation measurements. The lateral extent of the fault segments range from 5 to 10 km and make up a broad,45 km long, NW trending fault system. The geometry of each segment is quite simple and consists of planar faults gently dipping toward SW with an average dip of 40–45. The fault planes are not listric but maintain a constant dip through the entire seismogenic volume, down to 8 km depth. We observe the activation of faults on the hanging wall and the absence of seismicity in the footwall of the structure. The observed fault segmentation appears to be due to the lateral heterogeneity of the upper crust: preexisting thrusts inherited from Neogene’s compressional tectonic intersect the active normal faults and control their maximum length. The stress tensor obtained by inverting the six main shock focal mechanisms of the sequence is in agreement with the tectonic stress active in the inner chain of the Apennine, revealing a clear NE trending extension direction. Aftershock focal mechanisms show a consistent extensional kinematics, 70% of which are mechanically consistent with the main shock stress field.
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