Location

Location ANSS

The ANSS event ID is ak0097yfgadg and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/ak0097yfgadg/executive.

2009/06/22 19:28:05 61.939 -150.704 64.6 5.4 Alaska

Focal Mechanism

 USGS/SLU Moment Tensor Solution
 ENS  2009/06/22 19:28:05:0  61.94 -150.70  64.6 5.4 Alaska
 
 Stations used:
   AK.BRLK AK.CAST AK.CHUM AK.COLD AK.DIV AK.DOT AK.EYAK 
   AK.MCK AK.MDM AK.PAX AK.SAW AK.TRF AT.MID AT.OHAK AT.SVW2 
   US.EGAK 
 
 Filtering commands used:
   hp c 0.015 n 3
   lp c 0.04 n 3
 
 Best Fitting Double Couple
  Mo = 1.29e+24 dyne-cm
  Mw = 5.34 
  Z  = 63 km
  Plane   Strike  Dip  Rake
   NP1      141    58   -138
   NP2       25    55   -40
  Principal Axes:
   Axis    Value   Plunge  Azimuth
    T   1.29e+24      2     262
    N   0.00e+00     39     171
    P  -1.29e+24     51     355

 Moment Tensor: (dyne-cm)
    Component   Value
       Mxx    -4.80e+23
       Mxy     2.22e+23
       Mxz    -6.33e+23
       Myy     1.26e+24
       Myz     1.75e+22
       Mzz    -7.78e+23
                                                     
                                                     
                                                     
                                                     
                     --------------                  
                 --------------------##              
              #-----------------------####           
             ##------------------------####          
           ####-----------   ----------######        
          #####----------- P ----------#######       
         ######-----------   ----------########      
        #######------------------------#########     
        ########-----------------------#########     
       ##########---------------------###########    
       ###########--------------------###########    
         ##########------------------############    
       T ###########----------------#############    
         ############---------------############     
        ###############------------#############     
         ################--------##############      
          #################-----##############       
           ##################--##############        
             ################---###########          
              ############------------####           
                 ######----------------              
                     --------------                  
                                                     
                                                     
                                                     
 Global CMT Convention Moment Tensor:
      R          T          P
 -7.78e+23  -6.33e+23  -1.75e+22 
 -6.33e+23  -4.80e+23  -2.22e+23 
 -1.75e+22  -2.22e+23   1.26e+24 


Details of the solution is found at

http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20090622192805/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 = 25
      DIP = 55
     RAKE = -40
       MW = 5.34
       HS = 63.0

The NDK file is 20090622192805.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
USGSMT
AEIC
USGSCMT
 USGS/SLU Moment Tensor Solution
 ENS  2009/06/22 19:28:05:0  61.94 -150.70  64.6 5.4 Alaska
 
 Stations used:
   AK.BRLK AK.CAST AK.CHUM AK.COLD AK.DIV AK.DOT AK.EYAK 
   AK.MCK AK.MDM AK.PAX AK.SAW AK.TRF AT.MID AT.OHAK AT.SVW2 
   US.EGAK 
 
 Filtering commands used:
   hp c 0.015 n 3
   lp c 0.04 n 3
 
 Best Fitting Double Couple
  Mo = 1.29e+24 dyne-cm
  Mw = 5.34 
  Z  = 63 km
  Plane   Strike  Dip  Rake
   NP1      141    58   -138
   NP2       25    55   -40
  Principal Axes:
   Axis    Value   Plunge  Azimuth
    T   1.29e+24      2     262
    N   0.00e+00     39     171
    P  -1.29e+24     51     355

 Moment Tensor: (dyne-cm)
    Component   Value
       Mxx    -4.80e+23
       Mxy     2.22e+23
       Mxz    -6.33e+23
       Myy     1.26e+24
       Myz     1.75e+22
       Mzz    -7.78e+23
                                                     
                                                     
                                                     
                                                     
                     --------------                  
                 --------------------##              
              #-----------------------####           
             ##------------------------####          
           ####-----------   ----------######        
          #####----------- P ----------#######       
         ######-----------   ----------########      
        #######------------------------#########     
        ########-----------------------#########     
       ##########---------------------###########    
       ###########--------------------###########    
         ##########------------------############    
       T ###########----------------#############    
         ############---------------############     
        ###############------------#############     
         ################--------##############      
          #################-----##############       
           ##################--##############        
             ################---###########          
              ############------------####           
                 ######----------------              
                     --------------                  
                                                     
                                                     
                                                     
 Global CMT Convention Moment Tensor:
      R          T          P
 -7.78e+23  -6.33e+23  -1.75e+22 
 -6.33e+23  -4.80e+23  -2.22e+23 
 -1.75e+22  -2.22e+23   1.26e+24 


Details of the solution is found at

http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20090622192805/index.html
	
USGS Body-Wave Moment Tensor Solution

 09/06/22 19:28:04.27
 CENTRAL ALASKA                  
 Epicenter:  62.053 -150.840
 MW 5.4

 USGS MOMENT TENSOR SOLUTION
 Depth  65         No. of sta:  8
 Moment Tensor;   Scale 10**17 Nm
   Mrr=-1.35       Mtt= 0.62
   Mpp= 0.73       Mrt=-0.95
   Mrp= 0.26       Mtp=-0.84
  Principal axes:
   T  Val=  1.76  Plg=15  Azm=222
   N       -0.02      15      127
   P       -1.73      67      355

 Best Double Couple:Mo=1.7*10**17
  NP1:Strike=120 Dip=63 Slip=-108
  NP2:       334     32       -59
                                      
               #######                
          ------###########           
        -------------########         
      -----------------########       
    ---------------------########     
   #-----------------------#######    
   ##------------   --------######    
  ####----------- P ---------######   
  ######---------   ---------######   
  ########--------------------#####   
  ##########------------------#####   
  #############---------------#####   
   ###############------------####    
   ####################-------####    
    ####   ##################----     
      ## T ##################--       
           #################-         
          ################-           
               #######                
                                      


        

Moment tensor inversion summary for event 2009/06/22 19:28

Date: 2009/06/22
Time: 19:28 (UTC)
Region: Cook Inlet Region of Alaska
Mw=5.5

Location:

Lat.  61.9224;  Lon.  -150.6545; Depth   70 km 
(Best-fitting depth from moment tensor inversion)

Solution quality: poor
Number of stations = 6

Best Double Couple:

         strike    dip    rake 
Plane 1:  137.8   66.8  -139.3
Plane 2:   29.1   53.2   -29.5

Moment Tensor Parameters:

Mo = 1.74917e+24 dyn-cm
Mxx = -0.83; Mxy =  0.28; Mxz = -0.96
Myy =  1.64; Myz = -0.22; Mzz = -0.81


Principal Axes:

     value   azimuth   plunge
T:    1.72   260.59    8.34
N:    0.06   162.39   44.17
P:   -1.78   358.91   44.63

USGS Centroid Moment Tensor Solution

 09/06/22 19:28:04.27
 CENTRAL ALASKA                  
 Epicenter:  62.053 -150.840
 MW 5.5

 USGS CENTROID MOMENT TENSOR
 09/06/22 19:28:18.59
 Centroid:   62.153 -151.143
 Depth  51         No. of sta:118
 Moment Tensor;   Scale 10**17 Nm
   Mrr=-0.81       Mtt=-0.59
   Mpp= 1.39       Mrt=-1.20
   Mrp= 0.20       Mtp=-0.82
  Principal axes:
   T  Val=  1.85  Plg=14  Azm=244
   N        0.10      41      140
   P       -1.95      44      349

 Best Double Couple:Mo=1.9*10**17
  NP1:Strike= 16 Dip=47 Slip= -25
  NP2:       124     72      -133
                                      
               -------                
          --------------###           
        -----------------####         
      ---------   --------#####       
    ----------- P ---------######     
   ###---------   ---------#######    
   ####--------------------#######    
  #######------------------########   
  #########----------------########   
  ###########--------------########   
  #############-----------#########   
  ##   ###########--------#########   
   # T ##############----#########    
   #   #################-#########    
    ###################---------#     
      ################---------       
        ############---------         
          #######----------           
               -------                
                                      


        

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:

hp c 0.015 n 3
lp c 0.04 n 3
The results of this grid search are as follow:

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96   40.0    20    50   -35   5.17 0.4940
WVFGRD96   41.0    20    50   -35   5.18 0.5019
WVFGRD96   42.0    20    55   -40   5.20 0.5094
WVFGRD96   43.0    20    55   -40   5.21 0.5167
WVFGRD96   44.0    20    55   -40   5.21 0.5235
WVFGRD96   45.0    20    55   -40   5.22 0.5299
WVFGRD96   46.0    20    55   -40   5.23 0.5359
WVFGRD96   47.0    20    55   -40   5.23 0.5414
WVFGRD96   48.0    20    55   -40   5.24 0.5465
WVFGRD96   49.0    20    55   -40   5.25 0.5513
WVFGRD96   50.0    20    55   -40   5.26 0.5556
WVFGRD96   51.0    20    55   -40   5.26 0.5598
WVFGRD96   52.0    20    55   -40   5.27 0.5634
WVFGRD96   53.0    20    55   -40   5.27 0.5666
WVFGRD96   54.0    20    55   -40   5.28 0.5693
WVFGRD96   55.0    20    55   -45   5.29 0.5719
WVFGRD96   56.0    20    55   -45   5.30 0.5742
WVFGRD96   57.0    20    55   -45   5.31 0.5761
WVFGRD96   58.0    20    55   -45   5.31 0.5776
WVFGRD96   59.0    20    55   -45   5.32 0.5785
WVFGRD96   60.0    25    55   -40   5.32 0.5797
WVFGRD96   61.0    25    55   -40   5.33 0.5806
WVFGRD96   62.0    25    55   -40   5.33 0.5811
WVFGRD96   63.0    25    55   -40   5.34 0.5811
WVFGRD96   64.0    25    55   -40   5.34 0.5807
WVFGRD96   65.0    25    55   -40   5.35 0.5798
WVFGRD96   66.0    25    55   -40   5.35 0.5784
WVFGRD96   67.0    25    55   -40   5.36 0.5765
WVFGRD96   68.0    25    55   -40   5.36 0.5742
WVFGRD96   69.0    25    55   -40   5.36 0.5714

The best solution is

WVFGRD96   63.0    25    55   -40   5.34 0.5811

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

hp c 0.015 n 3
lp c 0.04 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 01:08:36 PM CDT 2024