Location

2006/05/20 07:05:56 37.65N 14.95E 12 4.1 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
 2006/05/20 07:05:56 37.65N 14.95E 12 4.1 Italy
 
 Best Fitting Double Couple
    Mo = 4.27e+21 dyne-cm
    Mw = 3.72 
    Z  = 23 km
     Plane   Strike  Dip  Rake
      NP1       85    65   -60
      NP2      211    38   -137
 Principal Axes:
   Axis    Value   Plunge  Azimuth
     T   4.27e+21     15     154
     N   0.00e+00     27     251
     P  -4.27e+21     59      38



 Moment Tensor: (dyne-cm)
    Component  Value
       Mxx     2.47e+21
       Mxy    -2.15e+21
       Mxz    -2.44e+21
       Myy     3.57e+20
       Myz    -6.91e+20
       Mzz    -2.83e+21
                                                     
                                                     
                                                     
                                                     
                     ##############                  
                 ###############-------              
              #############---------------           
             ###########-------------------          
           ##########------------------------        
          ##########--------------------------       
         #########-------------   -------------      
        #########-------------- P --------------     
        ########---------------   --------------     
       ########----------------------------------    
       #######----------------------------------#    
       #######--------------------------------###    
       --#####----------------------------#######    
        ------------------------------##########     
        -----##########---######################     
         -----#################################      
          ----################################       
           ---###############################        
             --####################   #####          
              --################### T ####           
                 ##################   #              
                     ##############                  
                                                     
                                                     
                                                     

 Harvard Convention
 Moment Tensor:
      R          T          F
 -2.83e+21  -2.44e+21   6.91e+20 
 -2.44e+21   2.47e+21   2.15e+21 
  6.91e+20   2.15e+21   3.57e+20 


Details of the solution is found at

http://www.eas.slu.edu/Earthquake_Center/NEW/20060520070556/index.html
        

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 = 85
      DIP = 65
     RAKE = -60
       MW = 3.72
       HS = 23

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   250    45   -80   3.35 0.0514
WVFGRD96    1.0    65    45   -90   3.38 0.0514
WVFGRD96    2.0   250    45   -80   3.45 0.0584
WVFGRD96    3.0    90    30    30   3.44 0.0633
WVFGRD96    4.0    85    35    20   3.45 0.0662
WVFGRD96    5.0   295    80    65   3.50 0.0756
WVFGRD96    6.0   290    80    60   3.51 0.0842
WVFGRD96    7.0   290    80    60   3.53 0.0940
WVFGRD96    8.0   290    80    60   3.56 0.1006
WVFGRD96    9.0   290    80    55   3.57 0.1061
WVFGRD96   10.0   290    80    55   3.58 0.1118
WVFGRD96   11.0   290    80    50   3.58 0.1150
WVFGRD96   12.0   105    90   -50   3.58 0.1186
WVFGRD96   13.0   100    85   -50   3.59 0.1207
WVFGRD96   14.0    95    75   -50   3.61 0.1229
WVFGRD96   15.0    90    70   -55   3.63 0.1277
WVFGRD96   16.0    90    70   -55   3.63 0.1294
WVFGRD96   17.0    90    70   -55   3.63 0.1312
WVFGRD96   18.0    90    65   -55   3.64 0.1339
WVFGRD96   19.0    90    65   -55   3.64 0.1346
WVFGRD96   20.0    90    65   -55   3.64 0.1357
WVFGRD96   21.0    85    65   -60   3.71 0.1410
WVFGRD96   22.0    90    65   -55   3.71 0.1413
WVFGRD96   23.0    85    65   -60   3.72 0.1416
WVFGRD96   24.0    90    65   -55   3.72 0.1410
WVFGRD96   25.0    90    65   -55   3.73 0.1403
WVFGRD96   26.0    85    60   -60   3.74 0.1393
WVFGRD96   27.0    90    65   -55   3.73 0.1368
WVFGRD96   28.0    90    65   -55   3.74 0.1359
WVFGRD96   29.0    90    65   -50   3.75 0.1342
WVFGRD96   30.0    90    65   -50   3.75 0.1321

The best solution is

WVFGRD96   23.0    85    65   -60   3.72 0.1416

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
CEL        50  107 iP_D
CLTB      268  153 eP_X
WDD       191  202 eP_-
TIP        42  232 eP_+
CUC        16  271 iP_D
MCRV        3  348 eP_X
SNAL        3  364 eP_-
CAFE        4  376 iP_C
AMUR       21  389 eP_X
NOCI       27  393 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 2006/05/20