Location

Location ANSS

The ANSS event ID is ld2010062300 and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/ld2010062300/executive.

2010/06/23 17:41:42 45.883 -75.475 18.9 5.35 Quebec

Focal Mechanism

 USGS/SLU Moment Tensor Solution
 ENS  2010/06/23 17:41:42:0  45.88  -75.47  18.9 5.3 Quebec
 
 Stations used:
   CN.A11 CN.A16 CN.A54 CN.A61 CN.A64 CN.GGN CN.KAPO CN.KGNO 
   CN.LMQ CN.SADO CN.VLDQ IU.HRV LD.ACCN LD.BRNY LD.HCNY 
   LD.KSPA LD.MMNY LD.NPNY LD.ODNJ LD.PAL LD.PRNY LD.PTN 
   LD.UCCT LD.WCNY NE.BRYW NE.FFD NE.HNH NE.QUA2 NE.TRY NE.WES 
   NE.WVL NE.YLE PE.PSWB PO.BANO PO.BMRO PO.BRCO PO.BUKO 
   PO.BWLO PO.CLWO PO.TOBO US.LONY US.NCB 
 
 Filtering commands used:
   cut o DIST/3.3 -30 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 = 3.98e+23 dyne-cm
  Mw = 5.00 
  Z  = 22 km
  Plane   Strike  Dip  Rake
   NP1      150    50    80
   NP2      345    41   102
  Principal Axes:
   Axis    Value   Plunge  Azimuth
    T   3.98e+23     81       7
    N   0.00e+00      8     156
    P  -3.98e+23      5     247

 Moment Tensor: (dyne-cm)
    Component   Value
       Mxx    -5.07e+22
       Mxy    -1.41e+23
       Mxz     7.25e+22
       Myy    -3.35e+23
       Myz     3.67e+22
       Mzz     3.86e+23
                                                     
                                                     
                                                     
                                                     
                     #####---------                  
                 ############----------              
              ---###############----------           
             ---##################---------          
           -----###################----------        
          -----######################---------       
         ------#######################---------      
        --------#######################---------     
        --------###########   #########---------     
       ---------########### T ##########---------    
       ----------##########   ##########---------    
       ----------########################--------    
       -----------#######################--------    
        -----------######################-------     
           ---------####################--------     
         P -----------##################-------      
           ------------#################------       
           --------------##############------        
             --------------###########-----          
              ----------------#######-----           
                 ------------------#---              
                     -------------#                  
                                                     
                                                     
                                                     
 Global CMT Convention Moment Tensor:
      R          T          P
  3.86e+23   7.25e+22  -3.67e+22 
  7.25e+22  -5.07e+22   1.41e+23 
 -3.67e+22   1.41e+23  -3.35e+23 


Details of the solution is found at

http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20100623174142/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 = 150
      DIP = 50
     RAKE = 80
       MW = 5.00
       HS = 22.0

The NDK file is 20100623174142.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.

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 +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    1.0    90    40   -90   4.72 0.5768
WVFGRD96    2.0    80    40   -90   4.80 0.5935
WVFGRD96    3.0   280    60   -55   4.85 0.5670
WVFGRD96    4.0   110    80   -55   4.83 0.5481
WVFGRD96    5.0   115    90   -55   4.82 0.5659
WVFGRD96    6.0   115    90   -55   4.82 0.5874
WVFGRD96    7.0   115    90   -55   4.82 0.6077
WVFGRD96    8.0   115    90   -55   4.82 0.6246
WVFGRD96    9.0   115    90   -50   4.82 0.6394
WVFGRD96   10.0   110    85   -55   4.85 0.6515
WVFGRD96   11.0   110    85   -55   4.85 0.6623
WVFGRD96   12.0   110    85   -55   4.85 0.6711
WVFGRD96   13.0   295    90    55   4.86 0.6775
WVFGRD96   14.0   310    65    55   4.90 0.6956
WVFGRD96   15.0   315    55    55   4.92 0.7131
WVFGRD96   16.0   315    55    55   4.93 0.7275
WVFGRD96   17.0   315    55    55   4.94 0.7390
WVFGRD96   18.0   150    55    80   4.95 0.7481
WVFGRD96   19.0   150    55    80   4.96 0.7557
WVFGRD96   20.0   150    55    80   4.99 0.7607
WVFGRD96   21.0   150    50    80   4.99 0.7633
WVFGRD96   22.0   150    50    80   5.00 0.7636
WVFGRD96   23.0   150    50    80   5.00 0.7617
WVFGRD96   24.0   310    55    50   5.01 0.7624
WVFGRD96   25.0   310    55    50   5.01 0.7584
WVFGRD96   26.0   315    50    55   5.02 0.7532
WVFGRD96   27.0   315    50    55   5.02 0.7466
WVFGRD96   28.0   315    50    55   5.03 0.7390
WVFGRD96   29.0   315    50    55   5.04 0.7301

The best solution is

WVFGRD96   22.0   150    50    80   5.00 0.7636

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 +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 CUS.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
CUS Model with Q from simple gamma values
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
  1.0000  5.0000  2.8900  2.5000 0.172E-02 0.387E-02 0.00  0.00  1.00  1.00 
  9.0000  6.1000  3.5200  2.7300 0.160E-02 0.363E-02 0.00  0.00  1.00  1.00 
 10.0000  6.4000  3.7000  2.8200 0.149E-02 0.336E-02 0.00  0.00  1.00  1.00 
 20.0000  6.7000  3.8700  2.9020 0.000E-04 0.000E-04 0.00  0.00  1.00  1.00 
  0.0000  8.1500  4.7000  3.3640 0.194E-02 0.431E-02 0.00  0.00  1.00  1.00 
Last Changed Sat Apr 27 12:16:18 PM CDT 2024