Page 260 - Numerical Analysis and Modelling in Geomechanics
P. 260

F.PERGALANI, V.PETRINI, A.PUGLIESE AND T.SANÒ 241
                                       Application


                       Some characteristics of The Umbria-Marche seismic
                                        sequence
            The  seismic  sequence  started  in  the  Umbria-Marche  Apennine  region  on  4
            September 1997 with an ML 4.4 earthquake located near the village of Colfiorito,
            close  to  the  boundary  between  the  Marche  and  Umbria  regions.  Several
            aftershocks with magnitude lower than 4 followed in the subsequent weeks. On
            26  September  at  00.33  GMT,  an  Ms  5.5  earthquake  occurred  with  epicentre
            located between the villages of Cesi and Colfiorito. It was followed by a stronger
            earthquake  at  09.40  GMT  (Ms  5.9;  Mw  6.0;  Table  8.1),  which  represents  the
            largest earthquake of the entire seismic sequence and caused damage as large as
            IX on the MCS macroseismic intensity scale. The epicentre was located north of
            the previous one, between the villages of Colfiorito and Annifo. A few minutes
            later  a  third  shock  occurred  (ML  4.7)  located  more  northward.  Strong  ground
            motion accelerographs of the National Electric Company, recorded peak ground
            accelerations as high as 0.5g at the
            Table 8.1 Main earthquakes (ML≥ 5) of the Umbria-Marche sequence (Pergalani et al.,
            1999)















            village of Nocera Umbra in both the main earthquakes. In the following weeks
            the  seismic  activity  was  very  high  with  more  than  2000  shocks  between  26
            September and 11 October with about 20 earthquakes exceeding magnitude 4 up
            to 14 October. Table 8.1 gives a list of earthquakes with magnitude greater than
            or equal to 5.
              It is interesting to note the migration of the seismic activity during the entire
            sequence.  Up  to  12  October,  the  seismic  activity,  which  was  initially
            concentrated  in  the  northern  part  of  the  area  (Figure  8.12),  migrated  to  the
            southern part, between the villages of Sellano and Preci, where on 14 October, at
            15.23 GMT an earthquake of Ms 5.5 occurred. Finally, in March and April 1998,
            two earthquakes with magnitude greater than 5 occurred more than 20 km north
            of the first sequence (Table 8.1). This activity seems to highlight the activation
   255   256   257   258   259   260   261   262   263   264   265