2015/10/29 00:37:47 42.24 3.18 10 4.5 Slovenia
USGS Felt map for this earthquake
USGS/SLU Moment Tensor Solution
ENS 2015/10/29 00:37:47:0 42.24 3.18 10.0 4.5 Slovenia
Stations used:
CH.GIMEL ES.EARA ES.EARI ES.ECHI ES.EIBI ES.EJON ES.ELAN
ES.EMOS ES.EORO ES.EPOB ES.ERTA ES.ETOS FR.ATE FR.BSTF
FR.CFF FR.FILF FR.FNEB FR.MLS FR.MONQ FR.OG35 FR.OGGM
FR.OGSM FR.PYLO FR.RUSF FR.SAUF FR.SJAF FR.TRBF FR.URDF
FR.VIEF G.SSB RD.MTLF RD.ORIF
Filtering commands used:
cut o DIST/3.3 -30 o DIST/3.3 +70
rtr
taper w 0.1
hp c 0.02 n 3
lp c 0.06 n 3
Best Fitting Double Couple
Mo = 9.55e+21 dyne-cm
Mw = 3.92
Z = 12 km
Plane Strike Dip Rake
NP1 200 75 20
NP2 105 71 164
Principal Axes:
Axis Value Plunge Azimuth
T 9.55e+21 25 63
N 0.00e+00 65 235
P -9.55e+21 3 332
Moment Tensor: (dyne-cm)
Component Value
Mxx -5.76e+21
Mxy 7.17e+21
Mxz 1.22e+21
Myy 4.13e+21
Myz 3.45e+21
Mzz 1.63e+21
--------------
P -------------######
--- ------------##########
-----------------#############
------------------################
------------------##################
------------------############## ###
------------------############### T ####
------------------############### ####
###---------------########################
######-----------#########################
#########--------#########################
##############--##########################
###############---######################
##############---------------#####------
#############-------------------------
###########-------------------------
##########------------------------
########----------------------
#######---------------------
####------------------
--------------
Global CMT Convention Moment Tensor:
R T P
1.63e+21 1.22e+21 -3.45e+21
1.22e+21 -5.76e+21 -7.17e+21
-3.45e+21 -7.17e+21 4.13e+21
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.EU/20151029003747/index.html
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STK = 200
DIP = 75
RAKE = 20
MW = 3.92
HS = 12.0
The NDK file is 20151029003747.ndk The waveform inversion is preferred.
The following compares this source inversion to others
USGS/SLU Moment Tensor Solution
ENS 2015/10/29 00:37:47:0 42.24 3.18 10.0 4.5 Slovenia
Stations used:
CH.GIMEL ES.EARA ES.EARI ES.ECHI ES.EIBI ES.EJON ES.ELAN
ES.EMOS ES.EORO ES.EPOB ES.ERTA ES.ETOS FR.ATE FR.BSTF
FR.CFF FR.FILF FR.FNEB FR.MLS FR.MONQ FR.OG35 FR.OGGM
FR.OGSM FR.PYLO FR.RUSF FR.SAUF FR.SJAF FR.TRBF FR.URDF
FR.VIEF G.SSB RD.MTLF RD.ORIF
Filtering commands used:
cut o DIST/3.3 -30 o DIST/3.3 +70
rtr
taper w 0.1
hp c 0.02 n 3
lp c 0.06 n 3
Best Fitting Double Couple
Mo = 9.55e+21 dyne-cm
Mw = 3.92
Z = 12 km
Plane Strike Dip Rake
NP1 200 75 20
NP2 105 71 164
Principal Axes:
Axis Value Plunge Azimuth
T 9.55e+21 25 63
N 0.00e+00 65 235
P -9.55e+21 3 332
Moment Tensor: (dyne-cm)
Component Value
Mxx -5.76e+21
Mxy 7.17e+21
Mxz 1.22e+21
Myy 4.13e+21
Myz 3.45e+21
Mzz 1.63e+21
--------------
P -------------######
--- ------------##########
-----------------#############
------------------################
------------------##################
------------------############## ###
------------------############### T ####
------------------############### ####
###---------------########################
######-----------#########################
#########--------#########################
##############--##########################
###############---######################
##############---------------#####------
#############-------------------------
###########-------------------------
##########------------------------
########----------------------
#######---------------------
####------------------
--------------
Global CMT Convention Moment Tensor:
R T P
1.63e+21 1.22e+21 -3.45e+21
1.22e+21 -5.76e+21 -7.17e+21
-3.45e+21 -7.17e+21 4.13e+21
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.EU/20151029003747/index.html
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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:
cut o DIST/3.3 -30 o DIST/3.3 +70 rtr taper w 0.1 hp c 0.02 n 3 lp c 0.06 n 3The results of this grid search from 0.5 to 19 km depth are as follow:
DEPTH STK DIP RAKE MW FIT
WVFGRD96 1.0 190 85 -10 3.59 0.3603
WVFGRD96 2.0 195 85 -15 3.68 0.4610
WVFGRD96 3.0 195 85 -20 3.73 0.5128
WVFGRD96 4.0 15 90 20 3.76 0.5484
WVFGRD96 5.0 195 80 -20 3.78 0.5787
WVFGRD96 6.0 20 90 20 3.79 0.6021
WVFGRD96 7.0 200 75 25 3.84 0.6327
WVFGRD96 8.0 205 65 30 3.88 0.6595
WVFGRD96 9.0 205 65 30 3.90 0.6812
WVFGRD96 10.0 205 65 30 3.91 0.6918
WVFGRD96 11.0 205 65 25 3.92 0.6960
WVFGRD96 12.0 200 75 20 3.92 0.6963
WVFGRD96 13.0 200 75 20 3.93 0.6925
WVFGRD96 14.0 200 80 15 3.94 0.6855
WVFGRD96 15.0 25 60 15 3.96 0.6795
WVFGRD96 16.0 25 65 15 3.96 0.6733
WVFGRD96 17.0 25 65 15 3.96 0.6672
WVFGRD96 18.0 25 65 15 3.97 0.6601
WVFGRD96 19.0 25 70 15 3.97 0.6522
WVFGRD96 20.0 25 70 15 3.98 0.6448
WVFGRD96 21.0 25 70 15 3.98 0.6367
WVFGRD96 22.0 25 70 15 3.99 0.6275
WVFGRD96 23.0 25 70 15 4.00 0.6176
WVFGRD96 24.0 25 75 15 3.99 0.6074
WVFGRD96 25.0 25 75 10 4.01 0.5972
WVFGRD96 26.0 25 75 10 4.02 0.5861
WVFGRD96 27.0 25 80 10 4.01 0.5749
WVFGRD96 28.0 25 80 10 4.02 0.5634
WVFGRD96 29.0 25 80 10 4.03 0.5514
The best solution is
WVFGRD96 12.0 200 75 20 3.92 0.6963
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. 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 0.02 n 3 lp c 0.06 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. |
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:
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.
Should the national backbone of the USGS Advanced National Seismic System (ANSS) be implemented with an interstation separation of 300 km, it is very likely that an earthquake such as this would have been recorded at distances on the order of 100-200 km. This means that the closest station would have information on source depth and mechanism that was lacking here.
Dr. Harley Benz, USGS, provided the USGS USNSN digital data. The digital data used in this study were provided by Natural Resources Canada through their AUTODRM site http://www.seismo.nrcan.gc.ca/nwfa/autodrm/autodrm_req_e.php, and IRIS using their BUD interface.
Thanks also to the many seismic network operators whose dedication make this effort possible: University of Alaska, University of Washington, Oregon State University, University of Utah, Montana Bureas of Mines, UC Berkely, Caltech, UC San Diego, Saint L ouis University, Universityof Memphis, Lamont Doehrty Earth Observatory, Boston College, the Iris stations and the Transportable Array of EarthScope.
The WUS 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
Here we tabulate the reasons for not using certain digital data sets
The following stations did not have a valid response files:
DATE=Sun Nov 1 16:40:07 CST 2015