The ANSS event ID is us10006249 and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/us10006249/executive.
2016/07/09 02:04:28 36.464 -98.758 7.2 4.4 Oklahoma
USGS/SLU Moment Tensor Solution ENS 2016/07/09 02:04:28:0 36.46 -98.76 7.2 4.4 Oklahoma Stations used: GS.KAN01 GS.KAN05 GS.KAN06 GS.KAN08 GS.KAN10 GS.KAN12 GS.KAN13 GS.KAN14 GS.KAN16 GS.KAN17 GS.KS20 GS.KS21 GS.OK025 GS.OK029 GS.OK030 GS.OK031 GS.OK032 GS.OK033 GS.OK034 GS.OK035 N4.R32B N4.T35B N4.U38B OK.BCOK OK.CHOK OK.CROK OK.ELIS OK.FNO OK.GORE OK.HTCH OK.NOKA OK.OKCFA OK.U32A TA.TUL1 US.CBKS US.KSU1 Filtering commands used: cut o DIST/3.3 -20 o DIST/3.3 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.10 n 3 Best Fitting Double Couple Mo = 3.80e+22 dyne-cm Mw = 4.32 Z = 7 km Plane Strike Dip Rake NP1 46 85 -170 NP2 315 80 -5 Principal Axes: Axis Value Plunge Azimuth T 3.80e+22 4 180 N 0.00e+00 79 72 P -3.80e+22 11 271 Moment Tensor: (dyne-cm) Component Value Mxx 3.79e+22 Mxy 5.67e+20 Mxz -2.45e+21 Myy -3.67e+22 Myz 6.85e+21 Mzz -1.13e+21 ############## ###################### ############################ --###########################- -------#######################---- ----------###################------- --------------###############--------- -----------------###########------------ -------------------#######-------------- - ------------------####---------------- - P -------------------------------------- - ------------------###----------------- --------------------#######--------------- -----------------###########------------ ---------------##############----------- ------------##################-------- ---------#####################------ -----#########################---- -############################- ############################ ######### ########## ##### T ###### Global CMT Convention Moment Tensor: R T P -1.13e+21 -2.45e+21 -6.85e+21 -2.45e+21 3.79e+22 -5.67e+20 -6.85e+21 -5.67e+20 -3.67e+22 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20160709020428/index.html |
STK = 315 DIP = 80 RAKE = -5 MW = 4.32 HS = 7.0
The NDK file is 20160709020428.ndk The waveform inversion is preferred.
The following compares this source inversion to those provided by others. The purpose is to look for major differences and also to note slight differences that might be inherent to the processing procedure. For completeness the USGS/SLU solution is repeated from above.
USGS/SLU Moment Tensor Solution ENS 2016/07/09 02:04:28:0 36.46 -98.76 7.2 4.4 Oklahoma Stations used: GS.KAN01 GS.KAN05 GS.KAN06 GS.KAN08 GS.KAN10 GS.KAN12 GS.KAN13 GS.KAN14 GS.KAN16 GS.KAN17 GS.KS20 GS.KS21 GS.OK025 GS.OK029 GS.OK030 GS.OK031 GS.OK032 GS.OK033 GS.OK034 GS.OK035 N4.R32B N4.T35B N4.U38B OK.BCOK OK.CHOK OK.CROK OK.ELIS OK.FNO OK.GORE OK.HTCH OK.NOKA OK.OKCFA OK.U32A TA.TUL1 US.CBKS US.KSU1 Filtering commands used: cut o DIST/3.3 -20 o DIST/3.3 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.10 n 3 Best Fitting Double Couple Mo = 3.80e+22 dyne-cm Mw = 4.32 Z = 7 km Plane Strike Dip Rake NP1 46 85 -170 NP2 315 80 -5 Principal Axes: Axis Value Plunge Azimuth T 3.80e+22 4 180 N 0.00e+00 79 72 P -3.80e+22 11 271 Moment Tensor: (dyne-cm) Component Value Mxx 3.79e+22 Mxy 5.67e+20 Mxz -2.45e+21 Myy -3.67e+22 Myz 6.85e+21 Mzz -1.13e+21 ############## ###################### ############################ --###########################- -------#######################---- ----------###################------- --------------###############--------- -----------------###########------------ -------------------#######-------------- - ------------------####---------------- - P -------------------------------------- - ------------------###----------------- --------------------#######--------------- -----------------###########------------ ---------------##############----------- ------------##################-------- ---------#####################------ -----#########################---- -############################- ############################ ######### ########## ##### T ###### Global CMT Convention Moment Tensor: R T P -1.13e+21 -2.45e+21 -6.85e+21 -2.45e+21 3.79e+22 -5.67e+20 -6.85e+21 -5.67e+20 -3.67e+22 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20160709020428/index.html |
Regional Moment Tensor (Mwr) Moment 4.625e+15 N-m Magnitude 4.4 Mwr Depth 8.0 km Percent DC 71 % Half Duration – Catalog US Data Source US1 Contributor US1 Nodal Planes Plane Strike Dip Rake NP1 48 77 -164 NP2 315 74 -13 Principal Axes Axis Value Plunge Azimuth T 4.942e+15 N-m 2 181 N -0.716e+15 N-m 70 86 P -4.225e+15 N-m 20 272 |
Given the availability of digital waveforms for determination of the moment tensor, this section documents the added processing leading to mLg, if appropriate to the region, and ML by application of the respective IASPEI formulae. As a research study, the linear distance term of the IASPEI formula for ML is adjusted to remove a linear distance trend in residuals to give a regionally defined ML. The defined ML uses horizontal component recordings, but the same procedure is applied to the vertical components since there may be some interest in vertical component ground motions. Residual plots versus distance may indicate interesting features of ground motion scaling in some distance ranges. A residual plot of the regionalized magnitude is given as a function of distance and azimuth, since data sets may transcend different wave propagation provinces.
Left: mLg computed using the IASPEI formula. Center: mLg residuals versus epicentral distance ; the values used for the trimmed mean magnitude estimate are indicated.
Right: residuals as a function of distance and azimuth.
Left: ML computed using the IASPEI formula for Horizontal components. Center: 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.
Right: Residuals from new relation as a function of distance and azimuth.
Left: ML computed using the IASPEI formula for Vertical components (research). Center: 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.
Right: Residuals from new relation as a function of distance and azimuth.
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The focal mechanism was determined using broadband seismic waveforms. The location of the event (star) and the stations used for (red) 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's 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 -20 o DIST/3.3 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.10 n 3The results of this grid search are as follow:
DEPTH STK DIP RAKE MW FIT WVFGRD96 1.0 315 70 0 3.96 0.4034 WVFGRD96 2.0 135 85 -10 4.09 0.5458 WVFGRD96 3.0 135 90 10 4.15 0.6038 WVFGRD96 4.0 315 80 -10 4.20 0.6467 WVFGRD96 5.0 315 75 -5 4.25 0.6736 WVFGRD96 6.0 315 75 -5 4.28 0.6891 WVFGRD96 7.0 315 80 -5 4.32 0.6953 WVFGRD96 8.0 315 80 -5 4.35 0.6948 WVFGRD96 9.0 315 80 -5 4.38 0.6873 WVFGRD96 10.0 140 85 5 4.40 0.6738 WVFGRD96 11.0 140 85 5 4.42 0.6605 WVFGRD96 12.0 140 85 5 4.43 0.6446 WVFGRD96 13.0 140 85 5 4.45 0.6271 WVFGRD96 14.0 140 80 5 4.46 0.6094 WVFGRD96 15.0 135 85 5 4.47 0.5904 WVFGRD96 16.0 135 85 5 4.48 0.5701 WVFGRD96 17.0 135 80 5 4.49 0.5525 WVFGRD96 18.0 135 80 5 4.50 0.5342 WVFGRD96 19.0 135 80 5 4.50 0.5154 WVFGRD96 20.0 135 75 5 4.51 0.4995 WVFGRD96 21.0 135 70 0 4.52 0.4833 WVFGRD96 22.0 135 70 -5 4.52 0.4699 WVFGRD96 23.0 135 70 -5 4.53 0.4568 WVFGRD96 24.0 135 65 -5 4.53 0.4454 WVFGRD96 25.0 135 65 -5 4.54 0.4370 WVFGRD96 26.0 135 65 -5 4.54 0.4290 WVFGRD96 27.0 135 65 -5 4.55 0.4213 WVFGRD96 28.0 225 80 10 4.54 0.4199 WVFGRD96 29.0 225 80 10 4.55 0.4284
The best solution is
WVFGRD96 7.0 315 80 -5 4.32 0.6953
The mechanism corresponding 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, the velocity model used in the predictions may not be perfect and the epicentral parameters may be be off. 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 -20 o DIST/3.3 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.10 n 3
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Figure 3. Waveform comparison for selected depth. Red: observed; Blue - predicted. The time shift with respect to the model prediction is indicated. The percent of fit is also indicated. The time scale is relative to the first trace sample. |
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Focal mechanism sensitivity at the preferred depth. The red color indicates a very good fit to the waveforms. 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.
The WUS.model used for the waveform synthetic seismograms and for the surface wave eigenfunctions and dispersion is as follows (The format is in the model96 format of Computer Programs in Seismology).
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