Location

Location ANSS

The ANSS event ID is usp000hk5s and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/usp000hk5s/executive.

2010/09/04 00:23:11 62.860 -125.820 1.0 3.9 NWT, Canada

Focal Mechanism

 USGS/SLU Moment Tensor Solution
 ENS  2010/09/04 00:23:11:0  62.86 -125.82   1.0 3.9 NWT, Canada
 
 Stations used:
   AK.BAL AK.BESE AK.CTG AK.DCPH AK.PIN AT.SKAG AT.YKU2 
   CN.CLVN CN.COKN CN.DHRN CN.DLBC CN.HPLN CN.HYT CN.INK 
   CN.KUKN CN.SMPN CN.WHY CN.YKW3 CN.YUK5 US.EGAK US.WRAK 
 
 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 0.10 n 3 
 
 Best Fitting Double Couple
  Mo = 9.89e+21 dyne-cm
  Mw = 3.93 
  Z  = 11 km
  Plane   Strike  Dip  Rake
   NP1      310    85   -60
   NP2       49    30   -170
  Principal Axes:
   Axis    Value   Plunge  Azimuth
    T   9.89e+21     33      15
    N   0.00e+00     30     127
    P  -9.89e+21     42     248

 Moment Tensor: (dyne-cm)
    Component   Value
       Mxx     5.72e+21
       Mxy    -1.23e+20
       Mxz     6.18e+21
       Myy    -4.23e+21
       Myz     5.75e+21
       Mzz    -1.49e+21
                                                     
                                                     
                                                     
                                                     
                     ##############                  
                 ######################              
              ################   #########           
             ################# T ##########          
           ---################   ###########-        
          -------############################-       
         -----------#########################--      
        --------------#######################---     
        ----------------#####################---     
       --------------------##################----    
       ----------------------################----    
       ------------------------#############-----    
       --------   ---------------###########-----    
        ------- P -----------------########-----     
        -------   -------------------#####------     
         ------------------------------#-------      
          ----------------------------###-----       
           -------------------------#######--        
             ---------------------#########          
              ###------------#############           
                 ######################              
                     ##############                  
                                                     
                                                     
                                                     
 Global CMT Convention Moment Tensor:
      R          T          P
 -1.49e+21   6.18e+21  -5.75e+21 
  6.18e+21   5.72e+21   1.23e+20 
 -5.75e+21   1.23e+20  -4.23e+21 


Details of the solution is found at

http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20100904002311/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 = 310
      DIP = 85
     RAKE = -60
       MW = 3.93
       HS = 11.0

The NDK file is 20100904002311.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.

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 -40 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    0.5   295    60    65   3.83 0.5858
WVFGRD96    1.0   125    35    70   3.87 0.5980
WVFGRD96    2.0   135    30    90   3.97 0.5896
WVFGRD96    3.0   315    60    90   4.00 0.5392
WVFGRD96    4.0   140    80    65   3.91 0.5493
WVFGRD96    5.0   135    85    65   3.89 0.5776
WVFGRD96    6.0   135    85    60   3.89 0.6008
WVFGRD96    7.0   135    85    60   3.89 0.6194
WVFGRD96    8.0   135    90    60   3.89 0.6332
WVFGRD96    9.0   310    85   -55   3.90 0.6443
WVFGRD96   10.0   310    85   -60   3.93 0.6506
WVFGRD96   11.0   310    85   -60   3.93 0.6534
WVFGRD96   12.0   310    85   -60   3.94 0.6532
WVFGRD96   13.0   310    80   -60   3.95 0.6509
WVFGRD96   14.0   310    80   -55   3.97 0.6463
WVFGRD96   15.0   310    80   -55   3.98 0.6391
WVFGRD96   16.0   310    75   -60   3.99 0.6300
WVFGRD96   17.0   310    75   -60   3.99 0.6193
WVFGRD96   18.0   310    75   -60   4.00 0.6070
WVFGRD96   19.0   310    75   -60   4.01 0.5939
WVFGRD96   20.0   310    75   -60   4.04 0.5803
WVFGRD96   21.0   310    75   -60   4.05 0.5645
WVFGRD96   22.0   310    75   -60   4.06 0.5478
WVFGRD96   23.0   310    75   -60   4.07 0.5306
WVFGRD96   24.0   315    70   -60   4.08 0.5140
WVFGRD96   25.0   310    65   -65   4.09 0.4977
WVFGRD96   26.0   140    35   -85   4.09 0.4841
WVFGRD96   27.0   140    35   -85   4.09 0.4708
WVFGRD96   28.0   140    35   -85   4.10 0.4577
WVFGRD96   29.0   140    35   -85   4.11 0.4445

The best solution is

WVFGRD96   11.0   310    85   -60   3.93 0.6534

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 -40 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.

Surface-Wave Focal Mechanism

The following figure shows the stations used in the grid search for the best focal mechanism to fit the surface-wave spectral amplitudes of the Love and Rayleigh waves.
Location of broadband stations used to obtain focal mechanism from surface-wave spectral amplitudes

The surface-wave determined focal mechanism is shown here.


  NODAL PLANES 

  
  STK=     326.51
  DIP=      60.50
 RAKE=      95.73
  
             OR
  
  STK=     135.00
  DIP=      30.00
 RAKE=      80.00
 
 
DEPTH = 6.0 km
 
Mw = 4.08
Best Fit 0.8033 - P-T axis plot gives solutions with FIT greater than FIT90

Surface-wave analysis

Surface wave analysis was performed using codes from Computer Programs in Seismology, specifically the multiple filter analysis program do_mft and the surface-wave radiation pattern search program srfgrd96.

Data preparation

Digital data were collected, instrument response removed and traces converted to Z, R an T components. Multiple filter analysis was applied to the Z and T traces to obtain the Rayleigh- and Love-wave spectral amplitudes, respectively. These were input to the search program which examined all depths between 1 and 25 km and all possible mechanisms.
Best mechanism fit as a function of depth. The preferred depth is given above. Lower hemisphere projection

Pressure-tension axis trends. Since the surface-wave spectra search does not distinguish between P and T axes and since there is a 180 ambiguity in strike, all possible P and T axes are plotted. First motion data and waveforms will be used to select the preferred mechanism. The purpose of this plot is to provide an idea of the possible range of solutions. The P and T-axes for all mechanisms with goodness of fit greater than 0.9 FITMAX (above) are plotted here.


Focal mechanism sensitivity at the preferred depth. The red color indicates a very good fit to the Love and Rayleigh wave radiation patterns. 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. Because of the symmetry of the spectral amplitude rediation patterns, only strikes from 0-180 degrees are sampled.

Love-wave radiation patterns

Rayleigh-wave radiation patterns