Location

Location ANSS

The ANSS event ID is usb000tike and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/usb000tike/executive.

2015/01/27 11:31:10 36.262 -97.264 3.4 4.2 Kansas

Focal Mechanism

USGS/SLU Moment Tensor Solution ENS 2015/01/27 11:31:10:0 36.26 -97.26 3.4 4.2 Kansas Stations used: AG.FCAR AG.HHAR AG.WHAR AG.WLAR GS.KAN01 GS.KAN08 GS.KAN10 GS.KAN11 GS.KAN12 GS.KAN13 GS.KAN14 GS.KS21 GS.OK025 GS.OK026 GS.OK027 GS.OK028 GS.OK029 GS.OK030 GS.OK031 N4.N33B N4.P38B N4.R32B N4.R40B N4.S39B N4.T35B N4.U38B N4.Z35B N4.Z38B NM.MGMO NM.UALR OK.BCOK OK.CROK OK.FNO OK.QUOK OK.U32A OK.X37A TA.ABTX TA.TUL1 TA.U40A TA.W39A TA.WHTX TA.X40A US.AMTX US.CBKS US.KSU1 US.MIAR US.WMOK Filtering commands used: cut o DIST/3.3 -30 o DIST/3.3 +70 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.06 n 3 Best Fitting Double Couple Mo = 2.88e+22 dyne-cm Mw = 4.24 Z = 4 km Plane Strike Dip Rake NP1 285 90 5 NP2 195 85 180 Principal Axes: Axis Value Plunge Azimuth T 2.88e+22 4 150 N 0.00e+00 85 285 P -2.88e+22 4 60 Moment Tensor: (dyne-cm) Component Value Mxx 1.44e+22 Mxy -2.49e+22 Mxz -2.43e+21 Myy -1.44e+22 Myz -6.51e+20 Mzz -2.20e+14 ############-- ###############------- ##################---------- ##################------------ ###################-------------- ####################-------------- P ####################--------------- #####################------------------- ---#################-------------------- -----------#########---------------------- ------------------##---------------------- -------------------#####------------------ -------------------############----------- -----------------####################--- -----------------####################### ----------------###################### --------------###################### -------------##################### -----------################### ---------############# ### ------############# T --############ Global CMT Convention Moment Tensor: R T P -2.20e+14 -2.43e+21 6.51e+20 -2.43e+21 1.44e+22 2.49e+22 6.51e+20 2.49e+22 -1.44e+22 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20150127113110/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 = 285
      DIP = 90
     RAKE = 5
       MW = 4.24
       HS = 4.0

The NDK file is 20150127113110.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 M_L by application of the respective IASPEI formulae. As a research study, the linear distance term of the IASPEI formula for M_L is adjusted to remove a linear distance trend in residuals to give a regionally defined M_L. The defined M_L 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 +70
rtr
taper w 0.1
hp c 0.03 n 3 
lp c 0.06 n 3

The results of this grid search are as follow:

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96    1.0   285    80     0   4.07 0.4681
WVFGRD96    2.0   285    90     5   4.16 0.5490
WVFGRD96    3.0   285    90     5   4.21 0.5754
WVFGRD96    4.0   285    90     5   4.24 0.5792
WVFGRD96    5.0   285    85     5   4.26 0.5712
WVFGRD96    6.0   285    80     5   4.29 0.5581
WVFGRD96    7.0   285    80     5   4.31 0.5435
WVFGRD96    8.0   285    70     5   4.34 0.5284
WVFGRD96    9.0   285    70     5   4.35 0.5122
WVFGRD96   10.0   290    75    15   4.36 0.4984
WVFGRD96   11.0   290    75    15   4.37 0.4860
WVFGRD96   12.0   290    75    15   4.37 0.4748
WVFGRD96   13.0   290    75    15   4.38 0.4644
WVFGRD96   14.0   290    70    10   4.39 0.4549
WVFGRD96   15.0   290    70    10   4.40 0.4462
WVFGRD96   16.0   290    75    10   4.40 0.4383
WVFGRD96   17.0   290    75    10   4.41 0.4312
WVFGRD96   18.0   290    75    10   4.41 0.4248
WVFGRD96   19.0   290    75    10   4.42 0.4190
WVFGRD96   20.0   290    75    10   4.43 0.4139
WVFGRD96   21.0   290    75    15   4.43 0.4094
WVFGRD96   22.0   290    75    15   4.44 0.4050
WVFGRD96   23.0   290    75    15   4.45 0.4010
WVFGRD96   24.0   290    75    15   4.45 0.3975
WVFGRD96   25.0   290    75    15   4.46 0.3941
WVFGRD96   26.0   290    75    15   4.47 0.3911
WVFGRD96   27.0   290    75    15   4.47 0.3880
WVFGRD96   28.0   290    75    15   4.48 0.3849
WVFGRD96   29.0   290    75    15   4.49 0.3816

The best solution is

WVFGRD96    4.0   285    90     5   4.24 0.5792

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 +70
rtr
taper w 0.1
hp c 0.03 n 3 
lp c 0.06 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:

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.

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 Fri Apr 26 01:25:22 PM CDT 2024