Location

2005/08/22 12:02:08 41.44N 12.50E 30 4.7 Italy

Arrival Times (from USGS)

Arrival time list

Felt Map

USGS Felt map for this earthquake

USGS Felt reports page for Intermountain Western US

Focal Mechanism

 SLU Moment Tensor Solution
 2005/08/22 12:02:08 41.44N 12.50E 30 4.7 Italy
 
 Best Fitting Double Couple
    Mo = 1.10e+23 dyne-cm
    Mw = 4.66 
    Z  = 9 km
     Plane   Strike  Dip  Rake
      NP1      250    85    10
      NP2      159    80   175
 Principal Axes:
   Axis    Value   Plunge  Azimuth
     T   1.10e+23     11     115
     N   0.00e+00     79     276
     P  -1.10e+23      3      24



 Moment Tensor: (dyne-cm)
    Component  Value
       Mxx    -7.21e+22
       Mxy    -8.13e+22
       Mxz    -1.44e+22
       Myy     6.88e+22
       Myz     1.53e+22
       Mzz     3.31e+21
                                                     
                                                     
                                                     
                                                     
                     --------------                  
                 ####-------------- P -              
              #######--------------   ----           
             ########----------------------          
           ###########-----------------------        
          ############------------------------       
         ##############------------------------      
        ###############----------------------###     
        ################--------------##########     
       #################--------#################    
       ##################--######################    
       ###############----#######################    
       ##########---------#######################    
        #####--------------#####################     
        ##------------------###############   ##     
         --------------------############## T #      
          --------------------#############          
           --------------------##############        
             -------------------###########          
              -------------------#########           
                 -----------------#####              
                     --------------                  
                                                     
                                                     
                                                     

 Harvard Convention
 Moment Tensor:
      R          T          F
  3.31e+21  -1.44e+22  -1.53e+22 
 -1.44e+22  -7.21e+22   8.13e+22 
 -1.53e+22   8.13e+22   6.88e+22 


Details of the solution is found at

http://www.eas.slu.edu/Earthquake_Center/NEW/20050822120208/index.html
        
INGV Rapid Moment Tensor

The focal mechanism was determined using broadband seismic waveforms. The location of the event and the station distribution are given in Figure 1.
Figure 1. Location of broadband stations used to obtain focal mechanism

Preferred Solution

The preferred solution from an analysis of the surface-wave spectral amplitude radiation pattern, waveform inversion and first motion observations is

      STK = 250
      DIP = 85
     RAKE = 10
       MW = 4.66
       HS = 9

The solution given here is from waveform inversion of regional vaeforms from the INGV digital seismic stations.

Waveform Inversion

The program wvfgrd96 was used with good traces observed at short distance to determine the focal mechanism, depth and seismic moment. This technique requires a high quality signal and well determined velocity model for the Green functions. To the extent that these are the quality data, this type of mechanism should be preferred over the radiation pattern technique which requires the separate step of defining the pressure and tension quadrants and the correct strike.

The observed and predicted traces are filtered using the following gsac commands:

hp c 0.02 3
lp c 0.05 3
The results of this grid search from 0.5 to 19 km depth are as follow:

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96    0.5   245    70   -15   4.36 0.2351
WVFGRD96    1.0   245    75   -15   4.39 0.2555
WVFGRD96    2.0   245    75   -15   4.47 0.3167
WVFGRD96    3.0   245    80   -10   4.51 0.3528
WVFGRD96    4.0   245    85    -5   4.54 0.3778
WVFGRD96    5.0   245    85     5   4.57 0.3977
WVFGRD96    6.0   245    85     5   4.60 0.4171
WVFGRD96    7.0   250    80    10   4.62 0.4289
WVFGRD96    8.0   250    80    10   4.64 0.4363
WVFGRD96    9.0   250    85    10   4.66 0.4386
WVFGRD96   10.0   250    85    10   4.67 0.4367
WVFGRD96   11.0    70    80     0   4.68 0.4322
WVFGRD96   12.0    70    80     0   4.69 0.4306
WVFGRD96   13.0    70    75     0   4.70 0.4284
WVFGRD96   14.0    70    75    -5   4.71 0.4272
WVFGRD96   15.0    70    75    -5   4.72 0.4254
WVFGRD96   16.0    70    75    -5   4.73 0.4189
WVFGRD96   17.0    70    80    -5   4.73 0.4161
WVFGRD96   18.0    70    80    -5   4.74 0.4135
WVFGRD96   19.0    70    80    -5   4.75 0.4110
WVFGRD96   20.0    70    80    -5   4.76 0.4052
WVFGRD96   21.0    70    75    -5   4.77 0.4039
WVFGRD96   22.0    70    75    -5   4.78 0.4000
WVFGRD96   23.0    70    75    -5   4.78 0.3957
WVFGRD96   24.0    70    80    -5   4.79 0.3923
WVFGRD96   25.0    70    80    -5   4.79 0.3888
WVFGRD96   26.0    70    80    -5   4.80 0.3818
WVFGRD96   27.0    70    80    -5   4.80 0.3784
WVFGRD96   28.0    85    80   -30   4.79 0.3748
WVFGRD96   29.0    85    80   -30   4.79 0.3722
WVFGRD96   30.0    80    80   -30   4.81 0.3696

The best solution is

WVFGRD96    9.0   250    85    10   4.66 0.4386

The mechanism correspond to the best fit is
Figure 1. Waveform inversion focal mechanism

The best fit as a function of depth is given in the following figure:

Figure 2. Depth sensitivity for waveform mechanism

The comparison of the observed and predicted waveforms is given in the next figure. The red traces are the observed and the blue are the predicted. Each observed-predicted componnet is plotted to the same scale and peak amplitudes are indicated by the numbers to the left of each trace. The number in black at the rightr of each predicted traces it the time shift required for maximum correlation between the observed and predicted traces. This time shift is required because the synthetics are not computed at exactly the same distance as the observed and because the velocity model used in the predictions may not be perfect. A positive time shift indicates that the prediction is too fast and should be delayed to match the observed trace (shift to the right in this figure). A negative value indicates that the prediction is too slow. The bandpass filter used in the processing and for the display was

hp c 0.02 3
lp c 0.05 3
Figure 3. Waveform comparison for depth of 8 km
Focal mechanism sensitivity at the preferred depth. The red color indicates a very good fit to thewavefroms. Each solution is plotted as a vector at a given value of strike and dip with the angle of the vector representing the rake angle, measured, with respect to the upward vertical (N) in the figure.

First motion data

The P-wave first motion data for focal mechanism studies are as follow:

Sta Az(deg)    Dist(km)   First motion
ROM9        2   44 iP_C
CERT       35   70 eP_-
TOLF      329   81 iP_C
FIAM       29  106 iP_D
AQU        36  127 iP_D
INTR       61  133 eP_-
RNI2       77  141 eP_-
VAGA       90  145 eP_+
MIDA       80  148 eP_+
CII        77  154 eP_-
TERO       34  161 eP_-
SACS      343  165 eP_-
BSSO       85  175 eP_+
ARCI      332  179 eP_+
SACR       91  184 iP_C
FRES       71  190 iP_D
PSB1       96  195 iP_C
MURB        1  203 eP_X
MOCO       91  222 eP_X
CING       15  223 eP_-
CAFE      100  234 eP_-
SNAL      103  234 eP_X
MCRV      107  236 eP_X
MRLC      106  262 eP_-
VULT      101  267 eP_X
CUC       119  323 eP_+
FNVD      340  324 eP_X
BDI       333  331 eP_+
AMUR       98  349 eP_-
VLC       331  349 eP_+
NOCI       99  390 eP_+
TIP       123  440 eP_X
BOB       327  446 eP_+

Quality control

The follwoing stations were not used because of excessive low frequency noise in the deconvolved waveforms: AMUR, GIUL, RNI2, SNAL, TRIV

Last Changed 2005/08/22