USGS/SLU Moment Tensor Solution ENS 2022/09/09 18:51:30:0 64.75 -149.19 15.5 3.7 Alaska Stations used: AK.BPAW AK.CAST AK.CCB AK.E24K AK.F20K AK.G23K AK.H22K AK.H23K AK.H24K AK.HDA AK.I21K AK.I23K AK.I27K AK.J25K AK.J26L AK.MCK AK.MLY AK.NEA2 AK.PAX AK.POKR AK.RIDG AK.SCRK AK.WRH AT.PMR IM.IL31 IU.COLA Filtering commands used: cut o DIST/3.3 -40 o DIST/3.3 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.08 n 3 Best Fitting Double Couple Mo = 2.32e+21 dyne-cm Mw = 3.51 Z = 17 km Plane Strike Dip Rake NP1 20 90 15 NP2 290 75 180 Principal Axes: Axis Value Plunge Azimuth T 2.32e+21 11 246 N 0.00e+00 75 20 P -2.32e+21 11 154 Moment Tensor: (dyne-cm) Component Value Mxx -1.44e+21 Mxy 1.71e+21 Mxz 2.05e+20 Myy 1.44e+21 Myz -5.64e+20 Mzz -5.24e+13 -------------- -----------------##### --------------------######## --------------------########## ---------------------############# ----------------------############## ----------------------################ ###########-----------################## ##################----################## ######################--################## #####################--------############# #####################-----------########## ####################---------------####### ##################-------------------### ## #############---------------------# # T ############---------------------- ###########---------------------- #############--------------------- ##########-------------------- ########------------- ---- #####------------- P - -------------- Global CMT Convention Moment Tensor: R T P -5.24e+13 2.05e+20 5.64e+20 2.05e+20 -1.44e+21 -1.71e+21 5.64e+20 -1.71e+21 1.44e+21 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20220909185130/index.html |
STK = 20 DIP = 90 RAKE = 15 MW = 3.51 HS = 17.0
The NDK file is 20220909185130.ndk The waveform inversion is preferred.
The following compares this source inversion to others
USGS/SLU Moment Tensor Solution ENS 2022/09/09 18:51:30:0 64.75 -149.19 15.5 3.7 Alaska Stations used: AK.BPAW AK.CAST AK.CCB AK.E24K AK.F20K AK.G23K AK.H22K AK.H23K AK.H24K AK.HDA AK.I21K AK.I23K AK.I27K AK.J25K AK.J26L AK.MCK AK.MLY AK.NEA2 AK.PAX AK.POKR AK.RIDG AK.SCRK AK.WRH AT.PMR IM.IL31 IU.COLA Filtering commands used: cut o DIST/3.3 -40 o DIST/3.3 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.08 n 3 Best Fitting Double Couple Mo = 2.32e+21 dyne-cm Mw = 3.51 Z = 17 km Plane Strike Dip Rake NP1 20 90 15 NP2 290 75 180 Principal Axes: Axis Value Plunge Azimuth T 2.32e+21 11 246 N 0.00e+00 75 20 P -2.32e+21 11 154 Moment Tensor: (dyne-cm) Component Value Mxx -1.44e+21 Mxy 1.71e+21 Mxz 2.05e+20 Myy 1.44e+21 Myz -5.64e+20 Mzz -5.24e+13 -------------- -----------------##### --------------------######## --------------------########## ---------------------############# ----------------------############## ----------------------################ ###########-----------################## ##################----################## ######################--################## #####################--------############# #####################-----------########## ####################---------------####### ##################-------------------### ## #############---------------------# # T ############---------------------- ###########---------------------- #############--------------------- ##########-------------------- ########------------- ---- #####------------- P - -------------- Global CMT Convention Moment Tensor: R T P -5.24e+13 2.05e+20 5.64e+20 2.05e+20 -1.44e+21 -1.71e+21 5.64e+20 -1.71e+21 1.44e+21 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20220909185130/index.html |
(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.
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 -40 o DIST/3.3 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.08 n 3The results of this grid search are as follow:
DEPTH STK DIP RAKE MW FIT WVFGRD96 1.0 200 90 0 2.96 0.2717 WVFGRD96 2.0 20 90 10 3.09 0.3692 WVFGRD96 3.0 20 90 20 3.16 0.4060 WVFGRD96 4.0 20 90 25 3.21 0.4375 WVFGRD96 5.0 20 90 25 3.25 0.4695 WVFGRD96 6.0 20 90 25 3.28 0.5048 WVFGRD96 7.0 20 90 25 3.31 0.5428 WVFGRD96 8.0 20 90 25 3.36 0.5814 WVFGRD96 9.0 20 90 25 3.39 0.6143 WVFGRD96 10.0 20 90 25 3.41 0.6414 WVFGRD96 11.0 20 90 20 3.43 0.6648 WVFGRD96 12.0 20 90 20 3.44 0.6836 WVFGRD96 13.0 20 90 20 3.46 0.6972 WVFGRD96 14.0 20 90 15 3.48 0.7071 WVFGRD96 15.0 20 90 15 3.49 0.7149 WVFGRD96 16.0 200 90 -15 3.50 0.7193 WVFGRD96 17.0 20 90 15 3.51 0.7207 WVFGRD96 18.0 200 90 -15 3.52 0.7196 WVFGRD96 19.0 20 90 15 3.53 0.7172 WVFGRD96 20.0 20 90 15 3.54 0.7140 WVFGRD96 21.0 20 90 15 3.55 0.7098 WVFGRD96 22.0 20 90 15 3.55 0.7050 WVFGRD96 23.0 20 90 15 3.56 0.6996 WVFGRD96 24.0 200 90 -15 3.57 0.6940 WVFGRD96 25.0 20 90 15 3.57 0.6881 WVFGRD96 26.0 20 90 15 3.58 0.6817 WVFGRD96 27.0 20 90 15 3.59 0.6752 WVFGRD96 28.0 20 90 15 3.59 0.6680 WVFGRD96 29.0 20 90 15 3.60 0.6601
The best solution is
WVFGRD96 17.0 20 90 15 3.51 0.7207
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 -40 o DIST/3.3 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.08 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.
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 Bureau of Mines, UC Berkely, Caltech, UC San Diego, Saint Louis University, University of Memphis, Lamont Doherty Earth Observatory, the Oklahoma Geological Survey, TexNet, the Iris stations, the Transportable Array of EarthScope and other networks.
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
Here we tabulate the reasons for not using certain digital data sets
The following stations did not have a valid response files: