The ANSS event ID is us70008uim and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/us70008uim/executive.
2020/04/12 03:09:52 44.494 -115.151 10.0 3.9 Idaho
USGS/SLU Moment Tensor Solution ENS 2020/04/12 03:09:52:0 44.49 -115.15 10.0 3.9 Idaho Stations used: GS.ID11 IE.BCYI IW.DLMT IW.FLWY IW.FXWY IW.LOHW IW.MFID IW.MOOW IW.PLID IW.SNOW US.AHID US.BMO US.BOZ US.ELK US.HAWA US.HLID US.HWUT US.MSO US.WVOR UU.BGU UU.HVU UU.SPU WY.YDD WY.YHL WY.YMP WY.YNE 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 br c 0.12 0.25 n 4 p 2 Best Fitting Double Couple Mo = 7.50e+21 dyne-cm Mw = 3.85 Z = 11 km Plane Strike Dip Rake NP1 145 65 -35 NP2 251 59 -150 Principal Axes: Axis Value Plunge Azimuth T 7.50e+21 4 199 N 0.00e+00 48 294 P -7.50e+21 42 106 Moment Tensor: (dyne-cm) Component Value Mxx 6.32e+21 Mxy 3.45e+21 Mxz 5.41e+20 Myy -3.02e+21 Myz -3.75e+21 Mzz -3.29e+21 ############## ###################### --########################## ---########################### -----############################# ------############################## --------###########----------------### ----------#####------------------------- ----------#----------------------------- ---------###------------------------------ -------######----------------------------- -----#########----------------- -------- ---############---------------- P -------- -##############--------------- ------- #################----------------------- ##################-------------------- ##################------------------ ###################--------------- ####################---------- ######################------ ### ################ T ############ Global CMT Convention Moment Tensor: R T P -3.29e+21 5.41e+20 3.75e+21 5.41e+20 6.32e+21 -3.45e+21 3.75e+21 -3.45e+21 -3.02e+21 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20200412030952/index.html |
STK = 145 DIP = 65 RAKE = -35 MW = 3.85 HS = 11.0
The NDK file is 20200412030952.ndk The waveform inversion is preferred.
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: 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.
![]() |
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.
![]() |
|
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 -40 o DIST/3.3 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.08 n 3 br c 0.12 0.25 n 4 p 2The results of this grid search are as follow:
DEPTH STK DIP RAKE MW FIT WVFGRD96 1.0 345 75 15 3.51 0.5123 WVFGRD96 2.0 340 60 25 3.64 0.6632 WVFGRD96 3.0 340 60 25 3.68 0.6847 WVFGRD96 4.0 335 50 10 3.72 0.7088 WVFGRD96 5.0 330 55 -5 3.73 0.7424 WVFGRD96 6.0 145 65 -40 3.78 0.8017 WVFGRD96 7.0 140 60 -45 3.81 0.8393 WVFGRD96 8.0 140 60 -45 3.85 0.8528 WVFGRD96 9.0 140 60 -45 3.86 0.8766 WVFGRD96 10.0 140 60 -40 3.85 0.8825 WVFGRD96 11.0 145 65 -35 3.85 0.8839 WVFGRD96 12.0 145 65 -30 3.85 0.8812 WVFGRD96 13.0 145 65 -30 3.86 0.8769 WVFGRD96 14.0 145 65 -30 3.86 0.8691 WVFGRD96 15.0 150 70 -25 3.87 0.8618 WVFGRD96 16.0 150 70 -25 3.88 0.8523 WVFGRD96 17.0 150 70 -20 3.88 0.8428 WVFGRD96 18.0 150 70 -20 3.89 0.8330 WVFGRD96 19.0 150 70 -20 3.90 0.8218 WVFGRD96 20.0 150 70 -20 3.91 0.8095 WVFGRD96 21.0 150 70 -20 3.92 0.7960 WVFGRD96 22.0 150 70 -20 3.92 0.7805 WVFGRD96 23.0 150 70 -15 3.93 0.7653 WVFGRD96 24.0 150 70 -15 3.93 0.7493 WVFGRD96 25.0 150 70 -15 3.94 0.7321 WVFGRD96 26.0 150 70 -15 3.94 0.7136 WVFGRD96 27.0 150 70 -15 3.95 0.6944 WVFGRD96 28.0 150 70 -10 3.95 0.6764 WVFGRD96 29.0 150 70 -10 3.96 0.6583
The best solution is
WVFGRD96 11.0 145 65 -35 3.85 0.8839
The mechanism corresponding to the best fit is
![]() |
|
The best fit as a function of depth is given in the following figure:
![]() |
|
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 -40 o DIST/3.3 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.08 n 3 br c 0.12 0.25 n 4 p 2
![]() |
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. |
![]() |
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