Location

Location ANSS

2021/01/04 06:49:53 45.42 16.23 5.0 4.5 Croatia

Focal Mechanism

USGS/SLU Moment Tensor Solution ENS 2021/01/04 06:49:53:6 45.42 16.23 5.0 4.5 Croatia Stations used: AC.KBN BW.ALFT BW.BE1 BW.BGDS BW.BIB BW.GELB BW.GRMB BW.KW1 BW.MANZ BW.MGBB BW.MGS01 BW.MGS02 BW.MGS03 BW.MGS05 BW.PART BW.RJOB BW.RMOA BW.RNHA BW.RNON BW.ROTZ BW.RTBE BW.SCE BW.TON BW.ZUGS CH.ACB CH.BALST CH.BERGE CH.BERNI CH.BNALP CH.DAGMA CH.DAVOX CH.DIX CH.EMING CH.EMMET CH.FUORN CH.FUSIO CH.GRIMS CH.HAUIG CH.LKBD2 CH.LLS CH.METMA CH.MMK CH.MUGIO CH.MUO CH.MUTEZ CH.PANIX CH.PLONS CH.ROMAN CH.SGT05 CH.SLE CH.SULZ CH.VDL CH.VDR CH.WALHA CH.WGT CH.ZUR CR.ZAG GE.MATE GE.STU GR.BFO GR.BRG GR.CLL GR.FUR GR.GEC2 GR.GEC7 GR.GRA1 GR.GRA2 GR.GRA4 GR.GRB1 GR.GRB3 GR.GRB4 GR.GRC1 GR.GRC2 GR.GRC3 GR.GRC4 GR.MOX GR.UBR GR.WET HT.NEST HU.AMBH HU.BUD HU.KOVH HU.MORH HU.MPLH HU.SOP MN.BLY MN.DPC MN.PDG MN.TUE OE.ABTA OE.ARSA OE.BIOA OE.CONA OE.DAVA OE.FETA OE.KBA OE.LESA OE.MOA OE.MOTA OE.MYKA OE.OBKA OE.RETA OE.RONA OE.SOKA OE.SQTA OE.VIE OE.WATA OX.ACOM OX.AGOR OX.BAD OX.BALD OX.CAE OX.CIMO OX.CLUD OX.DRE OX.MARN OX.MLN OX.MPRI OX.SABO SJ.BBLS SJ.FRGS SL.BOJS SL.CADS SL.CEY SL.CRES SL.CRNS SL.DOBS SL.GBAS SL.GBRS SL.GCIS SL.GOLS SL.GORS SL.GROS SL.JAVS SL.KNDS SL.KOGS SL.LJU SL.MOZS SL.PDKS SL.PERS SL.ROBS SL.SKDS SL.VISS SL.VNDS SL.VOJS SL.ZAVS SX.TANN Filtering commands used: cut o DIST/3.3 -30 o DIST/3.3 +70 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.06 n 3 Best Fitting Double Couple Mo = 2.19e+22 dyne-cm Mw = 4.16 Z = 10 km Plane Strike Dip Rake NP1 265 50 60 NP2 127 48 121 Principal Axes: Axis Value Plunge Azimuth T 2.19e+22 67 108 N 0.00e+00 23 285 P -2.19e+22 1 16 Moment Tensor: (dyne-cm) Component Value Mxx -2.00e+22 Mxy -6.63e+21 Mxz -2.66e+21 Myy 1.31e+21 Myz 7.29e+21 Mzz 1.87e+22 ----------- P --------------- ---- ---------------------------- ------------------------------ ---------------------------------- #----------------------------------- ##--------#####################------- ####---#############################---- ####-#################################-- ####--###################################- ##-----################## ############## #-------################# T ############## ---------################ ############## ----------############################## ------------############################ -------------######################### ---------------##################### -----------------################# -----------------------###---- ---------------------------- ---------------------- -------------- Global CMT Convention Moment Tensor: R T P 1.87e+22 -2.66e+21 -7.29e+21 -2.66e+21 -2.00e+22 6.63e+21 -7.29e+21 6.63e+21 1.31e+21 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20210104064953/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 = 265
      DIP = 50
     RAKE = 60
       MW = 4.16
       HS = 10.0

The NDK file is 20210104064953.ndk The waveform inversion is preferred.

Moment Tensor Comparison

The following compares this source inversion to others

SLU

USGS/SLU Moment Tensor Solution ENS 2021/01/04 06:49:53:6 45.42 16.23 5.0 4.5 Croatia Stations used: AC.KBN BW.ALFT BW.BE1 BW.BGDS BW.BIB BW.GELB BW.GRMB BW.KW1 BW.MANZ BW.MGBB BW.MGS01 BW.MGS02 BW.MGS03 BW.MGS05 BW.PART BW.RJOB BW.RMOA BW.RNHA BW.RNON BW.ROTZ BW.RTBE BW.SCE BW.TON BW.ZUGS CH.ACB CH.BALST CH.BERGE CH.BERNI CH.BNALP CH.DAGMA CH.DAVOX CH.DIX CH.EMING CH.EMMET CH.FUORN CH.FUSIO CH.GRIMS CH.HAUIG CH.LKBD2 CH.LLS CH.METMA CH.MMK CH.MUGIO CH.MUO CH.MUTEZ CH.PANIX CH.PLONS CH.ROMAN CH.SGT05 CH.SLE CH.SULZ CH.VDL CH.VDR CH.WALHA CH.WGT CH.ZUR CR.ZAG GE.MATE GE.STU GR.BFO GR.BRG GR.CLL GR.FUR GR.GEC2 GR.GEC7 GR.GRA1 GR.GRA2 GR.GRA4 GR.GRB1 GR.GRB3 GR.GRB4 GR.GRC1 GR.GRC2 GR.GRC3 GR.GRC4 GR.MOX GR.UBR GR.WET HT.NEST HU.AMBH HU.BUD HU.KOVH HU.MORH HU.MPLH HU.SOP MN.BLY MN.DPC MN.PDG MN.TUE OE.ABTA OE.ARSA OE.BIOA OE.CONA OE.DAVA OE.FETA OE.KBA OE.LESA OE.MOA OE.MOTA OE.MYKA OE.OBKA OE.RETA OE.RONA OE.SOKA OE.SQTA OE.VIE OE.WATA OX.ACOM OX.AGOR OX.BAD OX.BALD OX.CAE OX.CIMO OX.CLUD OX.DRE OX.MARN OX.MLN OX.MPRI OX.SABO SJ.BBLS SJ.FRGS SL.BOJS SL.CADS SL.CEY SL.CRES SL.CRNS SL.DOBS SL.GBAS SL.GBRS SL.GCIS SL.GOLS SL.GORS SL.GROS SL.JAVS SL.KNDS SL.KOGS SL.LJU SL.MOZS SL.PDKS SL.PERS SL.ROBS SL.SKDS SL.VISS SL.VNDS SL.VOJS SL.ZAVS SX.TANN Filtering commands used: cut o DIST/3.3 -30 o DIST/3.3 +70 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.06 n 3 Best Fitting Double Couple Mo = 2.19e+22 dyne-cm Mw = 4.16 Z = 10 km Plane Strike Dip Rake NP1 265 50 60 NP2 127 48 121 Principal Axes: Axis Value Plunge Azimuth T 2.19e+22 67 108 N 0.00e+00 23 285 P -2.19e+22 1 16 Moment Tensor: (dyne-cm) Component Value Mxx -2.00e+22 Mxy -6.63e+21 Mxz -2.66e+21 Myy 1.31e+21 Myz 7.29e+21 Mzz 1.87e+22 ----------- P --------------- ---- ---------------------------- ------------------------------ ---------------------------------- #----------------------------------- ##--------#####################------- ####---#############################---- ####-#################################-- ####--###################################- ##-----################## ############## #-------################# T ############## ---------################ ############## ----------############################## ------------############################ -------------######################### ---------------##################### -----------------################# -----------------------###---- ---------------------------- ---------------------- -------------- Global CMT Convention Moment Tensor: R T P 1.87e+22 -2.66e+21 -7.29e+21 -2.66e+21 -2.00e+22 6.63e+21 -7.29e+21 6.63e+21 1.31e+21 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20210104064953/index.html

Magnitudes

ML Magnitude

(a) ML computed using the IASPEI formula for Horizontal components; (b) ML residuals computed using a modified IASPEI formula that accounts for path specific attenuation; the values used for the trimmed mean are indicated. The ML relation used for each figure is given at the bottom of each plot.

(a) ML computed using the IASPEI formula for Vertical components (research); (b) ML residuals computed using a modified IASPEI formula that accounts for path specific attenuation; the values used for the trimmed mean are indicated. The ML relation used for each figure is given at the bottom of each plot.

Context

The next figure presents the focal mechanism for this earthquake (red) in the context of other events (blue) in the SLU Moment Tensor Catalog which are within ± 0.5 degrees of the new event. This comparison is shown in the left panel of the figure. The right panel shows the inferred direction of maximum compressive stress and the type of faulting (green is strike-slip, red is normal, blue is thrust; oblique is shown by a combination of colors).

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 o DIST/3.3 -30 o DIST/3.3 +70
rtr
taper w 0.1
hp c 0.03 n 3 
lp c 0.06 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   245    90   -10   3.75 0.3471
WVFGRD96    2.0   245    90   -10   3.84 0.4235
WVFGRD96    3.0   245    90   -35   3.93 0.4516
WVFGRD96    4.0   250    75    45   4.00 0.4943
WVFGRD96    5.0   250    70    40   4.01 0.5362
WVFGRD96    6.0   255    65    45   4.04 0.5684
WVFGRD96    7.0   255    60    45   4.05 0.5902
WVFGRD96    8.0   265    55    60   4.14 0.6225
WVFGRD96    9.0   270    50    65   4.17 0.6375
WVFGRD96   10.0   265    50    60   4.16 0.6433
WVFGRD96   11.0   265    50    60   4.16 0.6398
WVFGRD96   12.0   260    50    55   4.16 0.6303
WVFGRD96   13.0   255    55    45   4.14 0.6189
WVFGRD96   14.0   250    60    35   4.13 0.6082
WVFGRD96   15.0   245    65    30   4.13 0.5978
WVFGRD96   16.0   245    65    30   4.13 0.5881
WVFGRD96   17.0   245    70    25   4.14 0.5780
WVFGRD96   18.0   245    70    25   4.15 0.5677
WVFGRD96   19.0   245    70    25   4.15 0.5568
WVFGRD96   20.0   245    70    25   4.16 0.5456
WVFGRD96   21.0   245    70    25   4.16 0.5365
WVFGRD96   22.0   245    85    25   4.17 0.5251
WVFGRD96   23.0   240    80   -20   4.18 0.5152
WVFGRD96   24.0   240    80   -20   4.19 0.5086
WVFGRD96   25.0   240    80   -20   4.19 0.5018
WVFGRD96   26.0   240    75   -20   4.20 0.4947
WVFGRD96   27.0   240    80   -20   4.20 0.4873
WVFGRD96   28.0   240    80   -20   4.21 0.4796
WVFGRD96   29.0   240    80   -20   4.21 0.4722

The best solution is

WVFGRD96   10.0   265    50    60   4.16 0.6433

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 o DIST/3.3 -30 o DIST/3.3 +70
rtr
taper w 0.1
hp c 0.03 n 3 
lp c 0.06 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

Acknowledgements

Thanks also to the many seismic network operators whose dedication make this effort possible: University of Nevada Reno, University of Alaska, University of Washington, Oregon State University, University of Utah, Montana Bureas of Mines, UC Berkely, Caltech, UC San Diego, Saint Louis University, University of Memphis, Lamont Doherty Earth Observatory, the Iris stations and the Transportable Array of EarthScope.

Velocity Model

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

MODEL.01
Model after     8 iterations
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
     1.9000     3.4065     2.0089     2.2150  0.302E-02  0.679E-02   0.00       0.00       1.00       1.00    
     6.1000     5.5445     3.2953     2.6089  0.349E-02  0.784E-02   0.00       0.00       1.00       1.00    
    13.0000     6.2708     3.7396     2.7812  0.212E-02  0.476E-02   0.00       0.00       1.00       1.00    
    19.0000     6.4075     3.7680     2.8223  0.111E-02  0.249E-02   0.00       0.00       1.00       1.00    
     0.0000     7.9000     4.6200     3.2760  0.164E-10  0.370E-10   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:

Last Changed Wed Jan 6 19:24:55 CST 2021