2010/08/28 07:08:03 42.845 12.661 8.0 4.0 Italy
USGS Felt map for this earthquake
USGS/SLU Moment Tensor Solution ENS 2010/08/28 07:08:03:0 42.85 12.66 8.0 4.0 Italy Stations used: IV.ARVD IV.ATFO IV.ATVO IV.CAFI IV.CAMP IV.CASP IV.CERA IV.CERT IV.CESI IV.CING IV.CRE IV.CRMI IV.CSNT IV.FAGN IV.FIAM IV.FRES IV.FSSB IV.GIUL IV.GUAR IV.GUMA IV.LATE IV.MAON IV.MCIV IV.MGAB IV.MIDA IV.MNS IV.MTCE IV.PARC IV.POFI IV.RDP IV.RMP IV.RSM IV.SACS IV.SNTG IV.TERO IV.TOLF IV.TRTR IV.VVLD Filtering commands used: hp c 0.02 n 3 lp c 0.10 n 3 Best Fitting Double Couple Mo = 1.66e+22 dyne-cm Mw = 4.08 Z = 6 km Plane Strike Dip Rake NP1 340 75 -90 NP2 160 15 -90 Principal Axes: Axis Value Plunge Azimuth T 1.66e+22 30 70 N 0.00e+00 -0 160 P -1.66e+22 60 250 Moment Tensor: (dyne-cm) Component Value Mxx 9.71e+20 Mxy 2.67e+21 Mxz 4.92e+21 Myy 7.33e+21 Myz 1.35e+22 Mzz -8.30e+21 ############## #-----################ ##--------################## #------------################# ##--------------################## ##----------------################## ##------------------################## ###-------------------########## ##### ##--------------------########## T ##### ###---------------------######### ###### ###----------------------################# ###--------- ----------################# ###--------- P -----------################ ###-------- -----------############### ###-----------------------############## ###----------------------############# ###----------------------########### ###---------------------########## ###-------------------######## ####-----------------####### ####--------------#### #####--------- Global CMT Convention Moment Tensor: R T P -8.30e+21 4.92e+21 -1.35e+22 4.92e+21 9.71e+20 -2.67e+21 -1.35e+22 -2.67e+21 7.33e+21 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.IT/20100828070803/index.html |
STK = 340 DIP = 75 RAKE = -90 MW = 4.08 HS = 6.0
The waveform inversion is preferred.
The following compares this source inversion to others
USGS/SLU Moment Tensor Solution ENS 2010/08/28 07:08:03:0 42.85 12.66 8.0 4.0 Italy Stations used: IV.ARVD IV.ATFO IV.ATVO IV.CAFI IV.CAMP IV.CASP IV.CERA IV.CERT IV.CESI IV.CING IV.CRE IV.CRMI IV.CSNT IV.FAGN IV.FIAM IV.FRES IV.FSSB IV.GIUL IV.GUAR IV.GUMA IV.LATE IV.MAON IV.MCIV IV.MGAB IV.MIDA IV.MNS IV.MTCE IV.PARC IV.POFI IV.RDP IV.RMP IV.RSM IV.SACS IV.SNTG IV.TERO IV.TOLF IV.TRTR IV.VVLD Filtering commands used: hp c 0.02 n 3 lp c 0.10 n 3 Best Fitting Double Couple Mo = 1.66e+22 dyne-cm Mw = 4.08 Z = 6 km Plane Strike Dip Rake NP1 340 75 -90 NP2 160 15 -90 Principal Axes: Axis Value Plunge Azimuth T 1.66e+22 30 70 N 0.00e+00 -0 160 P -1.66e+22 60 250 Moment Tensor: (dyne-cm) Component Value Mxx 9.71e+20 Mxy 2.67e+21 Mxz 4.92e+21 Myy 7.33e+21 Myz 1.35e+22 Mzz -8.30e+21 ############## #-----################ ##--------################## #------------################# ##--------------################## ##----------------################## ##------------------################## ###-------------------########## ##### ##--------------------########## T ##### ###---------------------######### ###### ###----------------------################# ###--------- ----------################# ###--------- P -----------################ ###-------- -----------############### ###-----------------------############## ###----------------------############# ###----------------------########### ###---------------------########## ###-------------------######## ####-----------------####### ####--------------#### #####--------- Global CMT Convention Moment Tensor: R T P -8.30e+21 4.92e+21 -1.35e+22 4.92e+21 9.71e+20 -2.67e+21 -1.35e+22 -2.67e+21 7.33e+21 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.IT/20100828070803/index.html |
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Quick Regional Centroid Moment Tensor http://earthquake.rm.ingv.it/qrcmt.php ![]() |
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.
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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 n 3 lp c 0.10 n 3The results of this grid search from 0.5 to 19 km depth are as follow:
DEPTH STK DIP RAKE MW FIT WVFGRD96 1.0 345 30 -90 3.87 0.3549 WVFGRD96 2.0 340 80 -90 4.01 0.4258 WVFGRD96 3.0 155 10 -95 3.99 0.5362 WVFGRD96 4.0 155 15 -95 3.97 0.5886 WVFGRD96 5.0 150 15 -100 4.08 0.6187 WVFGRD96 6.0 340 75 -90 4.08 0.6239 WVFGRD96 7.0 150 15 -100 4.07 0.6069 WVFGRD96 8.0 340 75 -80 4.02 0.5778 WVFGRD96 9.0 340 75 -80 4.02 0.5543 WVFGRD96 10.0 345 80 -80 4.02 0.5287 WVFGRD96 11.0 345 80 -80 4.03 0.5049 WVFGRD96 12.0 345 80 -80 4.03 0.4802 WVFGRD96 13.0 345 80 -80 4.03 0.4551 WVFGRD96 14.0 345 85 -80 4.04 0.4317 WVFGRD96 15.0 345 85 -80 4.08 0.4106 WVFGRD96 16.0 165 90 80 4.09 0.3847 WVFGRD96 17.0 165 85 75 4.10 0.3621 WVFGRD96 18.0 300 15 45 4.10 0.3412 WVFGRD96 19.0 310 15 55 4.11 0.3216 WVFGRD96 20.0 305 20 50 4.11 0.3031 WVFGRD96 21.0 310 20 55 4.11 0.2871 WVFGRD96 22.0 315 20 60 4.12 0.2722 WVFGRD96 23.0 310 25 55 4.12 0.2597 WVFGRD96 24.0 320 25 65 4.12 0.2497 WVFGRD96 25.0 330 30 75 4.12 0.2432 WVFGRD96 26.0 335 30 80 4.13 0.2393 WVFGRD96 27.0 325 30 70 4.13 0.2353 WVFGRD96 28.0 320 35 70 4.14 0.2300 WVFGRD96 29.0 165 70 -70 4.14 0.2246
The best solution is
WVFGRD96 6.0 340 75 -90 4.08 0.6239
The mechanism correspond to the best fit is
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The best fit as a function of depth is given in the following figure:
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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. 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 n 3 lp c 0.10 n 3
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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. |
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
Here we tabulate the reasons for not using certain digital data sets
The following stations did not have a valid response files:
DATE=Sat Aug 28 07:48:21 CDT 2010