Abstract
A long sequence of earthquakes, six with magnitudes between 5 and
6, struck Central Italy starting on September 26, 1997, causing severe
damages and loss of human lives. The seismogenic structure consists
of a NW-SE elongated fault zone extending for about 40 km. The focal
mechanisms of the largest shocks reveal normal faulting with NE-SW
extension perpendicular to the trend of the Apennines, consistently
with the Quaternary tectonic setting of the internal sector of the
belt and with previous earthquakes in adjacent regions. Preliminary
data on the main shocks and aftershocks show that extension in this
region of the Apennines is accomplished by normal faults dipping
at low angle (\~40 deg) to the southwest, and confined in the upper
\~8 km of the crust. These normal faults might have reactivated
thrust planes of the Pliocene compressional tectonics. The aftershock
distribution and the damage patterns also suggest that the three
main shocks ruptured distinct 5 to 15 km-long fault segments, adjacent
and slightly offset from one another.
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