Location

2013/08/14 22:18:55 44.166 10.195 6.5 3.6 Italy

Arrival Times (from USGS)

Felt Map

Focal Mechanism

SLU Moment Tensor Solution ENS 2013/08/14 22:18:55:0 44.17 10.19 6.5 3.6 Italy Stations used: GU.FINB GU.GORR GU.MAIM GU.PCP GU.POPM IV.ARCI IV.ASQU IV.BDI IV.BOB IV.CAFI IV.CASP IV.CELB IV.CRMI IV.IMI IV.MSSA IV.OSSC IV.PARC IV.PLMA IV.QLNO IV.ZCCA MN.VLC Filtering commands used: cut a -10 a 60 rtr taper w 0.1 hp c 0.02 n 3 lp c 0.10 n 3 Best Fitting Double Couple Mo = 2.32e+21 dyne-cm Mw = 3.51 Z = 5 km Plane Strike Dip Rake NP1 238 57 -130 NP2 115 50 -45 Principal Axes: Axis Value Plunge Azimuth T 2.32e+21 4 355 N 0.00e+00 33 262 P -2.32e+21 57 91 Moment Tensor: (dyne-cm) Component Value Mxx 2.29e+21 Mxy -1.89e+20 Mxz 1.87e+20 Myy -6.73e+20 Myz -1.07e+21 Mzz -1.61e+21 #### T ####### ######## ########### ############################ ############################## ###########################---#### ####################---------------- #################--------------------- --#############------------------------- --##########---------------------------- ----#######------------------------------- -----####------------------- ----------- ------##-------------------- P ----------- ------##-------------------- ----------- ----#####------------------------------- ----#######----------------------------- --###########------------------------- -###############------------------## ################################## ############################## ############################ ###################### ############## Global CMT Convention Moment Tensor: R T P -1.61e+21 1.87e+20 1.07e+21 1.87e+20 2.29e+21 1.89e+20 1.07e+21 1.89e+20 -6.73e+20 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.IT/20130814221855/index.html

Preferred Solution

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

      STK = 115
      DIP = 50
     RAKE = -45
       MW = 3.51
       HS = 5.0

The NDK file is 20130814221855.ndk The waveform inversion is preferred.

Moment Tensor Comparison

The following compares this source inversion to others

SLU

SLU Moment Tensor Solution ENS 2013/08/14 22:18:55:0 44.17 10.19 6.5 3.6 Italy Stations used: GU.FINB GU.GORR GU.MAIM GU.PCP GU.POPM IV.ARCI IV.ASQU IV.BDI IV.BOB IV.CAFI IV.CASP IV.CELB IV.CRMI IV.IMI IV.MSSA IV.OSSC IV.PARC IV.PLMA IV.QLNO IV.ZCCA MN.VLC Filtering commands used: cut a -10 a 60 rtr taper w 0.1 hp c 0.02 n 3 lp c 0.10 n 3 Best Fitting Double Couple Mo = 2.32e+21 dyne-cm Mw = 3.51 Z = 5 km Plane Strike Dip Rake NP1 238 57 -130 NP2 115 50 -45 Principal Axes: Axis Value Plunge Azimuth T 2.32e+21 4 355 N 0.00e+00 33 262 P -2.32e+21 57 91 Moment Tensor: (dyne-cm) Component Value Mxx 2.29e+21 Mxy -1.89e+20 Mxz 1.87e+20 Myy -6.73e+20 Myz -1.07e+21 Mzz -1.61e+21 #### T ####### ######## ########### ############################ ############################## ###########################---#### ####################---------------- #################--------------------- --#############------------------------- --##########---------------------------- ----#######------------------------------- -----####------------------- ----------- ------##-------------------- P ----------- ------##-------------------- ----------- ----#####------------------------------- ----#######----------------------------- --###########------------------------- -###############------------------## ################################## ############################## ############################ ###################### ############## Global CMT Convention Moment Tensor: R T P -1.61e+21 1.87e+20 1.07e+21 1.87e+20 2.29e+21 1.89e+20 1.07e+21 1.89e+20 -6.73e+20 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.IT/20130814221855/index.html

Waveform Inversion

The focal mechanism was determined using broadband seismic waveforms. The location of the event and the and stations used for the waveform inversion are shown in the next figure.

Location of broadband stations used for 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:

cut a -10 a 60
rtr
taper w 0.1
hp c 0.02 n 3 
lp c 0.10 n 3

The results of this grid search from 0.5 to 19 km depth are as follow:

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96    1.0   120    35   -15   3.34 0.3783
WVFGRD96    2.0   120    35   -20   3.41 0.4394
WVFGRD96    3.0   115    45   -40   3.42 0.4883
WVFGRD96    4.0   115    50   -45   3.45 0.5150
WVFGRD96    5.0   115    50   -45   3.51 0.5187
WVFGRD96    6.0   115    55   -45   3.52 0.5105
WVFGRD96    7.0   120    60   -45   3.53 0.4904
WVFGRD96    8.0   125    65   -35   3.50 0.4689
WVFGRD96    9.0   125    70   -35   3.51 0.4487
WVFGRD96   10.0   125    70   -35   3.52 0.4294
WVFGRD96   11.0   130    70   -25   3.52 0.4095
WVFGRD96   12.0   130    70   -25   3.52 0.3934
WVFGRD96   13.0   135    65    25   3.51 0.3845
WVFGRD96   14.0   135    65    25   3.52 0.3748
WVFGRD96   15.0   135    65    30   3.54 0.3682
WVFGRD96   16.0   135    65    30   3.55 0.3618
WVFGRD96   17.0   135    65    30   3.55 0.3547
WVFGRD96   18.0   135    65    30   3.56 0.3465
WVFGRD96   19.0   135    65    30   3.57 0.3384
WVFGRD96   20.0   135    65    30   3.57 0.3304
WVFGRD96   21.0   135    65    30   3.57 0.3207
WVFGRD96   22.0   135    70    30   3.58 0.3126
WVFGRD96   23.0   135    70    25   3.59 0.3079
WVFGRD96   24.0   135    70    25   3.59 0.3036
WVFGRD96   25.0   140    65    30   3.61 0.3033
WVFGRD96   26.0   140    65    30   3.61 0.3020
WVFGRD96   27.0   140    65    30   3.63 0.3011
WVFGRD96   28.0   140    70    30   3.64 0.3010
WVFGRD96   29.0   145    65    35   3.66 0.2995

The best solution is

WVFGRD96    5.0   115    50   -45   3.51 0.5187

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 component is plotted to the same scale and peak amplitudes are indicated by the numbers to the left of each trace. A pair of numbers is given in black at the right of each predicted traces. The upper number 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 lower number gives the percentage of variance reduction to characterize the individual goodness of fit (100% indicates a perfect fit).

The bandpass filter used in the processing and for the display was

cut a -10 a 60
rtr
taper w 0.1
hp c 0.02 n 3 
lp c 0.10 n 3

Figure 3. Waveform comparison for selected depth

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.

A check on the assumed source location is possible by looking at the time shifts between the observed and predicted traces. The time shifts for waveform matching arise for several reasons:

The origin time and epicentral distance are incorrect
The velocity model used for the inversion is incorrect
The velocity model used to define the P-arrival time is not the same as the velocity model used for the waveform inversion (assuming that the initial trace alignment is based on the P arrival time)

Assuming only a mislocation, the time shifts are fit to a functional form:

 Time_shift = A + B cos Azimuth + C Sin Azimuth

The time shifts for this inversion lead to the next figure:

The derived shift in origin time and epicentral coordinates are given at the bottom of the figure.

Discussion

Velocity Model

The nnCIA used for the waveform synthetic seismograms and for the surface wave eigenfunctions and dispersion is as follows:

MODEL.01
C.It. A. Di Luzio et al Earth Plan Lettrs 280 (2009) 1-12 Fig 5. 7-8 MODEL/SURF3
ISOTROPIC
KGS
FLAT EARTH
1-D
CONSTANT VELOCITY
LINE08
LINE09
LINE10
LINE11
      H(KM)   VP(KM/S)   VS(KM/S) RHO(GM/CC)         QP         QS       ETAP       ETAS      FREFP      FREFS
     1.5000     3.7497     2.1436     2.2753  0.500E-02  0.100E-01   0.00       0.00       1.00       1.00    
     3.0000     4.9399     2.8210     2.4858  0.500E-02  0.100E-01   0.00       0.00       1.00       1.00    
     3.0000     6.0129     3.4336     2.7058  0.500E-02  0.100E-01   0.00       0.00       1.00       1.00    
     7.0000     5.5516     3.1475     2.6093  0.167E-02  0.333E-02   0.00       0.00       1.00       1.00    
    15.0000     5.8805     3.3583     2.6770  0.167E-02  0.333E-02   0.00       0.00       1.00       1.00    
     6.0000     7.1059     4.0081     3.0002  0.167E-02  0.333E-02   0.00       0.00       1.00       1.00    
     8.0000     7.1000     3.9864     3.0120  0.167E-02  0.333E-02   0.00       0.00       1.00       1.00    
     0.0000     7.9000     4.4036     3.2760  0.167E-02  0.333E-02   0.00       0.00       1.00       1.00

Quality Control

Here we tabulate the reasons for not using certain digital data sets

The following stations did not have a valid response files:

DATE=Wed Aug 14 19:22:18 CDT 2013

Last Changed 2013/08/14