Location

Location ANSS

The ANSS event ID is us2000dvlb and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/us2000dvlb/executive.

2018/04/06 15:07:12 36.285 -97.511 6.3 3.9 Oklahoma

Focal Mechanism

 USGS/SLU Moment Tensor Solution
 ENS  2018/04/06 15:07:12:0  36.28  -97.51   6.3 3.9 Oklahoma
 
 Stations used:
   AG.HHAR GM.IWM01 GS.OK029 GS.OK032 GS.OK033 GS.OK048 
   GS.OK052 N4.R32B N4.S39B N4.T35B N4.U38B O2.CHAN O2.DOVR 
   O2.DRUM O2.MRSH O2.PERK O2.PERY O2.POCA O2.SHWN OK.CHOK 
   OK.CROK OK.CSTR OK.DEOK OK.FNO OK.HTCH OK.W35A OK.X37A 
   TA.TUL3 US.CBKS 
 
 Filtering commands used:
   cut o DIST/3.3 -30 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 = 4.62e+21 dyne-cm
  Mw = 3.71 
  Z  = 5 km
  Plane   Strike  Dip  Rake
   NP1      150    90    10
   NP2       60    80   180
  Principal Axes:
   Axis    Value   Plunge  Azimuth
    T   4.62e+21      7      15
    N   0.00e+00     80     150
    P  -4.62e+21      7     285

 Moment Tensor: (dyne-cm)
    Component   Value
       Mxx     3.94e+21
       Mxy     2.28e+21
       Mxz     4.01e+20
       Myy    -3.94e+21
       Myz     6.95e+20
       Mzz    -7.02e+13
                                                     
                                                     
                                                     
                                                     
                     ########### T                   
                 -##############   ####              
              -----#######################           
             -------#######################          
           ----------########################        
          ------------########################       
         --------------#####################---      
           -------------##################------     
         P --------------###############--------     
       -   ---------------###########------------    
       --------------------#######---------------    
       ----------------------##------------------    
       ---------------------##-------------------    
        -----------------######-----------------     
        -------------###########----------------     
         --------################--------------      
          -#######################------------       
           ########################----------        
             #######################-------          
              #######################-----           
                 #####################-              
                     ##############                  
                                                     
                                                     
                                                     
 Global CMT Convention Moment Tensor:
      R          T          P
 -7.02e+13   4.01e+20  -6.95e+20 
  4.01e+20   3.94e+21  -2.28e+21 
 -6.95e+20  -2.28e+21  -3.94e+21 


Details of the solution is found at

http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20180406150712/index.html
        

Preferred Solution

The preferred solution from an analysis of the surface-wave spectral amplitude radiation pattern, waveform inversion or first motion observations is

      STK = 150
      DIP = 90
     RAKE = 10
       MW = 3.71
       HS = 5.0

The NDK file is 20180406150712.ndk The waveform inversion is preferred.

Magnitudes

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.

mLg Magnitude


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.

ML Magnitude


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.

Context

The left panel of the next figure presents the focal mechanism for this earthquake (red) in the context of other nearby events (blue) in the SLU Moment Tensor Catalog. The right panel shows the inferred direction of maximum compressive stress and the type of faulting (green is strike-slip, red is normal, blue is thrust; oblique is shown by a combination of colors). Thus context plot is useful for assessing the appropriateness of the moment tensor of this event.

Waveform Inversion using wvfgrd96

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.
Location of broadband stations used for waveform inversion

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 -30 o DIST/3.3 +50
rtr
taper w 0.1
hp c 0.03 n 3 
lp c 0.10 n 3 
The results of this grid search are as follow:

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96    1.0   325    75   -15   3.45 0.4547
WVFGRD96    2.0   150    90    20   3.58 0.5742
WVFGRD96    3.0   150    90    20   3.64 0.6344
WVFGRD96    4.0   150    90    15   3.68 0.6651
WVFGRD96    5.0   150    90    10   3.71 0.6757
WVFGRD96    6.0   330    85    -5   3.75 0.6741
WVFGRD96    7.0   330    85    -5   3.78 0.6655
WVFGRD96    8.0   325    85   -10   3.81 0.6509
WVFGRD96    9.0   325    85   -10   3.83 0.6305
WVFGRD96   10.0   145    90     5   3.84 0.6073
WVFGRD96   11.0   325    85    -5   3.86 0.5874
WVFGRD96   12.0   145    90     5   3.87 0.5651
WVFGRD96   13.0   325    90    -5   3.89 0.5433
WVFGRD96   14.0   145    90     5   3.90 0.5219
WVFGRD96   15.0   145    90     5   3.91 0.5015
WVFGRD96   16.0   145    90     5   3.92 0.4813
WVFGRD96   17.0   145    90     5   3.92 0.4626
WVFGRD96   18.0   145    90     5   3.93 0.4455
WVFGRD96   19.0   325    85    -5   3.94 0.4322
WVFGRD96   20.0   325    85    -5   3.94 0.4184
WVFGRD96   21.0   325    80    -5   3.95 0.4083
WVFGRD96   22.0   325    80    -5   3.95 0.4001
WVFGRD96   23.0   325    80    -5   3.96 0.3929
WVFGRD96   24.0   325    80    -5   3.96 0.3879
WVFGRD96   25.0   325    80    15   3.98 0.3846
WVFGRD96   26.0   325    90    25   3.99 0.3838
WVFGRD96   27.0   325    90    20   3.99 0.3829
WVFGRD96   28.0   325    90    20   3.99 0.3821
WVFGRD96   29.0    55    85    10   3.99 0.3772

The best solution is

WVFGRD96    5.0   150    90    10   3.71 0.6757

The mechanism corresponding to the best fit is
Figure 1. Waveform inversion focal mechanism

The best fit as a function of depth is given in the following figure:

Figure 2. Depth sensitivity for waveform mechanism

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 -30 o DIST/3.3 +50
rtr
taper w 0.1
hp c 0.03 n 3 
lp c 0.10 n 3 
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:

Assuming only a mislocation, the time shifts are fit to a functional form:

 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.

Velocity Model

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    
Last Changed Thu Apr 25 09:58:24 PM CDT 2024