Location

2014/07/09 02:10:04 37.069 -97.790 9.9 3.4 Kansas

Arrival Times (from USGS)

Felt Map

Focal Mechanism

USGS/SLU Moment Tensor Solution ENS 2014/07/09 02:10:04:0 37.07 -97.79 9.9 3.4 Kansas Stations used: GS.KAN10 GS.KAN11 GS.KAN12 GS.KAN13 N4.T35B OK.CROK OK.KAY1 Filtering commands used: cut o DIST/3.3 -20 o DIST/3.3 +30 rtr taper w 0.1 hp c 0.05 n 3 lp c 0.10 n 3 Best Fitting Double Couple Mo = 4.42e+20 dyne-cm Mw = 3.03 Z = 2 km Plane Strike Dip Rake NP1 205 85 65 NP2 104 25 168 Principal Axes: Axis Value Plunge Azimuth T 4.42e+20 44 90 N 0.00e+00 25 207 P -4.42e+20 35 316 Moment Tensor: (dyne-cm) Component Value Mxx -1.55e+20 Mxy 1.46e+20 Mxz -1.52e+20 Myy 8.53e+19 Myz 3.64e+20 Mzz 6.95e+19 -------------- -------------------### ---------------------####### ---------------------######### ------ -------------############ ------- P ------------############## -------- -----------################ ----------------------################## ---------------------################### #--------------------##################### #-------------------########### ######## ##-----------------############ T ######## ##----------------############# ######## ##---------------####################### ###-------------#######################- ####----------#######################- #####-------######################-- ######----#####################--- #######-##################---- ######-------#####---------- ###------------------- -------------- Global CMT Convention Moment Tensor: R T P 6.95e+19 -1.52e+20 -3.64e+20 -1.52e+20 -1.55e+20 -1.46e+20 -3.64e+20 -1.46e+20 8.53e+19 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20140709021004/index.html

Preferred Solution

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

      STK = 205
      DIP = 85
     RAKE = 65
       MW = 3.03
       HS = 2.0

The NDK file is 20140709021004.ndk The waveform inversion is preferred.

Moment Tensor Comparison

The following compares this source inversion to others

SLU

USGS/SLU Moment Tensor Solution ENS 2014/07/09 02:10:04:0 37.07 -97.79 9.9 3.4 Kansas Stations used: GS.KAN10 GS.KAN11 GS.KAN12 GS.KAN13 N4.T35B OK.CROK OK.KAY1 Filtering commands used: cut o DIST/3.3 -20 o DIST/3.3 +30 rtr taper w 0.1 hp c 0.05 n 3 lp c 0.10 n 3 Best Fitting Double Couple Mo = 4.42e+20 dyne-cm Mw = 3.03 Z = 2 km Plane Strike Dip Rake NP1 205 85 65 NP2 104 25 168 Principal Axes: Axis Value Plunge Azimuth T 4.42e+20 44 90 N 0.00e+00 25 207 P -4.42e+20 35 316 Moment Tensor: (dyne-cm) Component Value Mxx -1.55e+20 Mxy 1.46e+20 Mxz -1.52e+20 Myy 8.53e+19 Myz 3.64e+20 Mzz 6.95e+19 -------------- -------------------### ---------------------####### ---------------------######### ------ -------------############ ------- P ------------############## -------- -----------################ ----------------------################## ---------------------################### #--------------------##################### #-------------------########### ######## ##-----------------############ T ######## ##----------------############# ######## ##---------------####################### ###-------------#######################- ####----------#######################- #####-------######################-- ######----#####################--- #######-##################---- ######-------#####---------- ###------------------- -------------- Global CMT Convention Moment Tensor: R T P 6.95e+19 -1.52e+20 -3.64e+20 -1.52e+20 -1.55e+20 -1.46e+20 -3.64e+20 -1.46e+20 8.53e+19 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20140709021004/index.html

Magnitudes

mLg Magnitude

(a) mLg computed using the IASPEI formula; (b) mLg residuals ; the values used for the trimmed mean are indicated.

ML Magnitude

(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.

Context

The next figure presents the focal mechanism for this earthquake (red) in the context of other events (blue) in the SLU Moment Tensor Catalog which are within ± 0.5 degrees of the new event. This comparison is shown in the left panel of the figure. 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).

Waveform Inversion

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.

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 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 +30
rtr
taper w 0.1
hp c 0.05 n 3 
lp c 0.10 n 3

The results of this grid search from 0.5 to 19 km depth are as follow:

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96    1.0    15    90    65   2.87 0.3729
WVFGRD96    2.0   205    85    65   3.03 0.4144
WVFGRD96    3.0    15    90   -45   2.97 0.3991
WVFGRD96    4.0    95    60     5   2.99 0.3837
WVFGRD96    5.0    95    65    10   3.02 0.3867
WVFGRD96    6.0    95    65     5   3.04 0.3807
WVFGRD96    7.0   100    75    15   3.06 0.3724
WVFGRD96    8.0   100    75    25   3.12 0.3684
WVFGRD96    9.0   100    75    25   3.14 0.3637
WVFGRD96   10.0   100    75    25   3.16 0.3570
WVFGRD96   11.0   100    75    25   3.17 0.3499
WVFGRD96   12.0   100    80    30   3.20 0.3424
WVFGRD96   13.0   100    80    30   3.22 0.3348
WVFGRD96   14.0   100    80    25   3.22 0.3273
WVFGRD96   15.0   100    80    25   3.23 0.3205
WVFGRD96   16.0    95    80    20   3.24 0.3139
WVFGRD96   17.0    95    80    20   3.25 0.3076
WVFGRD96   18.0    95    80    20   3.27 0.3020
WVFGRD96   19.0    95    80    15   3.26 0.2963
WVFGRD96   20.0    95    80    15   3.27 0.2919
WVFGRD96   21.0    95    80    15   3.28 0.2884
WVFGRD96   22.0    95    85    25   3.31 0.2856
WVFGRD96   23.0    95    80    20   3.31 0.2865
WVFGRD96   24.0    95    80    25   3.34 0.2893
WVFGRD96   25.0    95    80    25   3.34 0.2941
WVFGRD96   26.0    95    85    25   3.35 0.2995
WVFGRD96   27.0    95    85    25   3.36 0.3039
WVFGRD96   28.0   270    90   -25   3.37 0.3081
WVFGRD96   29.0    95    80    20   3.36 0.3131

The best solution is

WVFGRD96    2.0   205    85    65   3.03 0.4144

The mechanism correspond 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 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 -20 o DIST/3.3 +30
rtr
taper w 0.1
hp c 0.05 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.

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:

The origin time and epicentral distance are incorrect
The velocity model used for the inversion is incorrect
The velocity model used to define the P-arrival time is not the same as the velocity model used for the waveform inversion (assuming that the initial trace alignment is based on the P arrival time)

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.

Discussion

Acknowledgements

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 Bureas of Mines, UC Berkely, Caltech, UC San Diego, Saint Louis University, University of Memphis, Lamont Doherty Earth Observatory, the Iris stations and the Transportable Array of EarthScope.

Velocity Model

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

Quality Control

Here we tabulate the reasons for not using certain digital data sets

The following stations did not have a valid response files:

Last Changed Mon Dec 7 00:13:20 CST 2015