Location

Location ANSS

The ANSS event ID is ak009ambz3p6 and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/ak009ambz3p6/executive.

2009/08/19 18:19:27 61.228 -150.858 66.4 5.1 Alaska

Focal Mechanism

 USGS/SLU Moment Tensor Solution
 ENS  2009/08/19 18:19:27:0  61.23 -150.86  66.4 5.1 Alaska
 
 Stations used:
   AK.BMR AK.CAST AK.CHUM AK.DIV AK.EYAK AK.MCK AK.PPLA AK.SAW 
   AK.SSN AK.TRF AT.PMR AT.SVW2 IU.COLA 
 
 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 0.07 n 3 
 
 Best Fitting Double Couple
  Mo = 2.82e+23 dyne-cm
  Mw = 4.90 
  Z  = 66 km
  Plane   Strike  Dip  Rake
   NP1      337    83   119
   NP2       80    30    15
  Principal Axes:
   Axis    Value   Plunge  Azimuth
    T   2.82e+23     45     276
    N   0.00e+00     29     153
    P  -2.82e+23     31      43

 Moment Tensor: (dyne-cm)
    Component   Value
       Mxx    -1.08e+23
       Mxy    -1.17e+23
       Mxz    -7.69e+22
       Myy     4.47e+22
       Myz    -2.26e+23
       Mzz     6.32e+22
                                                     
                                                     
                                                     
                                                     
                     --------------                  
                 ####------------------              
              ########--------------------           
             ##########--------------------          
           #############------------   ------        
          ###############----------- P -------       
         #################----------   --------      
        ###################---------------------     
        ####################--------------------     
       ########   ###########-------------------#    
       ######## T ############------------------#    
       ########   ############-----------------##    
       ########################----------------##    
        ########################--------------##     
        -########################-----------####     
         --######################----------####      
          ---#####################------######       
           -----##################----#######        
             -------#############--########          
              ---------------------#######           
                 -------------------###              
                     --------------                  
                                                     
                                                     
                                                     
 Global CMT Convention Moment Tensor:
      R          T          P
  6.32e+22  -7.69e+22   2.26e+23 
 -7.69e+22  -1.08e+23   1.17e+23 
  2.26e+23   1.17e+23   4.47e+22 


Details of the solution is found at

http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20090819181927/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 = 80
      DIP = 30
     RAKE = 15
       MW = 4.90
       HS = 66.0

The NDK file is 20090819181927.ndk The waveform inversion is preferred.

Moment Tensor Comparison

The following compares this source inversion to those provided by others. The purpose is to look for major differences and also to note slight differences that might be inherent to the processing procedure. For completeness the USGS/SLU solution is repeated from above.
SLU
AEIC
 USGS/SLU Moment Tensor Solution
 ENS  2009/08/19 18:19:27:0  61.23 -150.86  66.4 5.1 Alaska
 
 Stations used:
   AK.BMR AK.CAST AK.CHUM AK.DIV AK.EYAK AK.MCK AK.PPLA AK.SAW 
   AK.SSN AK.TRF AT.PMR AT.SVW2 IU.COLA 
 
 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 0.07 n 3 
 
 Best Fitting Double Couple
  Mo = 2.82e+23 dyne-cm
  Mw = 4.90 
  Z  = 66 km
  Plane   Strike  Dip  Rake
   NP1      337    83   119
   NP2       80    30    15
  Principal Axes:
   Axis    Value   Plunge  Azimuth
    T   2.82e+23     45     276
    N   0.00e+00     29     153
    P  -2.82e+23     31      43

 Moment Tensor: (dyne-cm)
    Component   Value
       Mxx    -1.08e+23
       Mxy    -1.17e+23
       Mxz    -7.69e+22
       Myy     4.47e+22
       Myz    -2.26e+23
       Mzz     6.32e+22
                                                     
                                                     
                                                     
                                                     
                     --------------                  
                 ####------------------              
              ########--------------------           
             ##########--------------------          
           #############------------   ------        
          ###############----------- P -------       
         #################----------   --------      
        ###################---------------------     
        ####################--------------------     
       ########   ###########-------------------#    
       ######## T ############------------------#    
       ########   ############-----------------##    
       ########################----------------##    
        ########################--------------##     
        -########################-----------####     
         --######################----------####      
          ---#####################------######       
           -----##################----#######        
             -------#############--########          
              ---------------------#######           
                 -------------------###              
                     --------------                  
                                                     
                                                     
                                                     
 Global CMT Convention Moment Tensor:
      R          T          P
  6.32e+22  -7.69e+22   2.26e+23 
 -7.69e+22  -1.08e+23   1.17e+23 
  2.26e+23   1.17e+23   4.47e+22 


Details of the solution is found at

http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20090819181927/index.html
	

Moment tensor inversion summary for event 2009/08/19 18:19

Date: 2009/08/19
Time: 18:19 (UTC)
Region: Cook Inlet Region of Alaska
Mw=5.1

Location:

Lat.  61.2286;  Lon.  -150.8254; Depth   70 km 
(Best-fitting depth from moment tensor inversion)

Solution quality: good;
Number of stations = 7

Best Double Couple:

         strike    dip    rake 
Plane 1:  174.0   87.0  -104.0
Plane 2:   72.3   14.3   -12.1

Moment Tensor Parameters:

Mo = 4.23092e+23 dyn-cm
Mxx = -0.19; Mxy = -0.96; Mxz = -0.48
Myy =  0.62; Myz = -4.05; Mzz = -0.43


Principal Axes:

     value   azimuth   plunge
T:    4.22   277.03   40.44
N:    0.01   174.77   14.00
P:   -4.23    69.71   46.19


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.

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 -40 o DIST/3.3 +50
rtr
taper w 0.1
hp c 0.03 n 3 
lp c 0.07 n 3 
The results of this grid search are as follow:

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96    2.0   320    45   -80   4.13 0.2620
WVFGRD96    4.0   330    75   -65   4.18 0.2239
WVFGRD96    6.0   325    75   -60   4.19 0.2617
WVFGRD96    8.0   325    75   -60   4.26 0.2805
WVFGRD96   10.0   230    35   -25   4.28 0.2987
WVFGRD96   12.0   240    40     0   4.29 0.3179
WVFGRD96   14.0   250    45    30   4.33 0.3392
WVFGRD96   16.0   255    40    30   4.35 0.3560
WVFGRD96   18.0   260    40    30   4.36 0.3700
WVFGRD96   20.0   260    40    30   4.39 0.3822
WVFGRD96   22.0   260    40    25   4.41 0.3917
WVFGRD96   24.0   260    40    25   4.43 0.4003
WVFGRD96   26.0   260    40    25   4.45 0.4071
WVFGRD96   28.0   255    40    20   4.47 0.4118
WVFGRD96   30.0   255    45    20   4.49 0.4142
WVFGRD96   32.0    50    55     0   4.55 0.4347
WVFGRD96   34.0    55    50     0   4.56 0.4602
WVFGRD96   36.0    55    50     0   4.59 0.4824
WVFGRD96   38.0    55    50     0   4.61 0.5016
WVFGRD96   40.0    55    35     0   4.72 0.5168
WVFGRD96   42.0    60    35     5   4.74 0.5430
WVFGRD96   44.0    65    35     5   4.76 0.5646
WVFGRD96   46.0    65    35     5   4.77 0.5818
WVFGRD96   48.0    60    35     5   4.79 0.6014
WVFGRD96   50.0    65    35     5   4.81 0.6240
WVFGRD96   52.0    70    30     5   4.83 0.6449
WVFGRD96   54.0    70    30    10   4.84 0.6640
WVFGRD96   56.0    70    30    10   4.85 0.6787
WVFGRD96   58.0    75    30    10   4.86 0.6915
WVFGRD96   60.0    75    30    10   4.87 0.7008
WVFGRD96   62.0    75    30    10   4.88 0.7073
WVFGRD96   64.0    75    30    15   4.89 0.7085
WVFGRD96   66.0    80    30    15   4.90 0.7102
WVFGRD96   68.0    85    25     5   4.92 0.7085
WVFGRD96   70.0    85    25     5   4.93 0.7048
WVFGRD96   72.0    85    25     5   4.94 0.7014
WVFGRD96   74.0    85    25     5   4.94 0.6939
WVFGRD96   76.0    85    25     5   4.94 0.6858
WVFGRD96   78.0    85    25     5   4.95 0.6759
WVFGRD96   80.0    90    25     5   4.96 0.6650
WVFGRD96   82.0    90    25     5   4.96 0.6542
WVFGRD96   84.0    90    25     5   4.96 0.6429
WVFGRD96   86.0    90    25     5   4.97 0.6304
WVFGRD96   88.0    95    25    10   4.96 0.6171
WVFGRD96   90.0    95    25    10   4.97 0.6037
WVFGRD96   92.0    95    25    10   4.97 0.5898
WVFGRD96   94.0    95    25    10   4.97 0.5766
WVFGRD96   96.0    95    25    10   4.97 0.5629
WVFGRD96   98.0   100    25    15   4.97 0.5503

The best solution is

WVFGRD96   66.0    80    30    15   4.90 0.7102

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 0.07 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 Sun Apr 28 01:08:52 PM CDT 2024