The ANSS event ID is nm607638 and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/nm607638/executive.
2010/10/14 10:07:34 35.299 -92.352 4.5 3.4 Arkansas
USGS/SLU Moment Tensor Solution
ENS 2010/10/14 10:07:34:0 35.30 -92.35 4.5 3.4 Arkansas
Stations used:
AG.FCAR AG.LCAR AG.WLAR NM.MGMO NM.UALR TA.S35A TA.S36A
TA.T35A TA.T37A TA.V34A TA.W36A TA.W37A TA.W38A TA.X37A
TA.X38A TA.Y36A TA.Y38A TA.Y39A TA.Z38A
Filtering commands used:
hp c 0.02 n 3
lp c 0.10 n 3
Best Fitting Double Couple
Mo = 1.53e+21 dyne-cm
Mw = 3.39
Z = 4 km
Plane Strike Dip Rake
NP1 115 90 -5
NP2 205 85 -180
Principal Axes:
Axis Value Plunge Azimuth
T 1.53e+21 4 160
N 0.00e+00 85 295
P -1.53e+21 4 70
Moment Tensor: (dyne-cm)
Component Value
Mxx 1.17e+21
Mxy -9.80e+20
Mxz -1.21e+20
Myy -1.17e+21
Myz -5.64e+19
Mzz 1.17e+13
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Global CMT Convention Moment Tensor:
R T P
1.17e+13 -1.21e+20 5.64e+19
-1.21e+20 1.17e+21 9.80e+20
5.64e+19 9.80e+20 -1.17e+21
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20101014100734/index.html
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STK = 115
DIP = 90
RAKE = -5
MW = 3.39
HS = 4.0
The NDK file is 20101014100734.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.
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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:
hp c 0.02 n 3 lp c 0.10 n 3The results of this grid search are as follow:
DEPTH STK DIP RAKE MW FIT
WVFGRD96 0.5 110 70 -10 3.30 0.2797
WVFGRD96 1.0 110 65 -10 3.34 0.2964
WVFGRD96 2.0 110 70 -15 3.37 0.3177
WVFGRD96 3.0 115 85 -5 3.38 0.3263
WVFGRD96 4.0 115 90 -5 3.39 0.3266
WVFGRD96 5.0 115 90 -5 3.40 0.3239
WVFGRD96 6.0 115 90 -5 3.41 0.3206
WVFGRD96 7.0 115 90 -5 3.42 0.3169
WVFGRD96 8.0 110 80 -10 3.42 0.3140
WVFGRD96 9.0 110 80 -10 3.43 0.3119
WVFGRD96 10.0 115 65 10 3.46 0.3113
WVFGRD96 11.0 115 65 10 3.47 0.3101
WVFGRD96 12.0 115 65 10 3.48 0.3079
WVFGRD96 13.0 115 65 10 3.48 0.3048
WVFGRD96 14.0 115 65 10 3.49 0.3020
WVFGRD96 15.0 115 70 10 3.50 0.2990
WVFGRD96 16.0 115 70 10 3.50 0.2959
WVFGRD96 17.0 115 70 10 3.51 0.2921
WVFGRD96 18.0 115 70 10 3.52 0.2885
WVFGRD96 19.0 115 65 10 3.53 0.2854
WVFGRD96 20.0 115 65 10 3.54 0.2828
WVFGRD96 21.0 115 65 10 3.55 0.2805
WVFGRD96 22.0 110 50 -15 3.59 0.2784
WVFGRD96 23.0 110 50 -15 3.60 0.2774
WVFGRD96 24.0 115 50 -5 3.61 0.2768
WVFGRD96 25.0 115 50 -5 3.62 0.2767
WVFGRD96 26.0 115 50 -5 3.62 0.2767
WVFGRD96 27.0 115 50 -5 3.63 0.2763
WVFGRD96 28.0 115 50 -5 3.64 0.2761
WVFGRD96 29.0 115 50 -5 3.64 0.2767
The best solution is
WVFGRD96 4.0 115 90 -5 3.39 0.3266
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
hp c 0.02 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 CUS.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 CUS Model with Q from simple gamma values 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 1.0000 5.0000 2.8900 2.5000 0.172E-02 0.387E-02 0.00 0.00 1.00 1.00 9.0000 6.1000 3.5200 2.7300 0.160E-02 0.363E-02 0.00 0.00 1.00 1.00 10.0000 6.4000 3.7000 2.8200 0.149E-02 0.336E-02 0.00 0.00 1.00 1.00 20.0000 6.7000 3.8700 2.9020 0.000E-04 0.000E-04 0.00 0.00 1.00 1.00 0.0000 8.1500 4.7000 3.3640 0.194E-02 0.431E-02 0.00 0.00 1.00 1.00