Location

Location SLU

To test the RMT solution P and S arrivals times wre manually picked as were P-wave first motions. The result of running elocate is given in elocate.txt. The RNT solution is superimposed on the first motions in the comparison below."

Location ANSS

2019/01/10 13:48:59 45.419 -66.251 5.0 3.8 New Brunswick, Canada

Focal Mechanism

 USGS/SLU Moment Tensor Solution
 ENS  2019/01/10 13:48:59:0  45.42  -66.25   5.0 3.8 New Brunswick, Canada
 
 Stations used:
   CN.GGN CN.HKNB CN.MCNB CN.SRNB N4.F64A N4.G65A 
 
 Filtering commands used:
   cut o DIST/3.3 -10 o DIST/3.3 +30
   rtr
   taper w 0.1
   hp c 0.10 n 3 
   lp c 0.50 n 3 
 
 Best Fitting Double Couple
  Mo = 1.64e+21 dyne-cm
  Mw = 3.41 
  Z  = 2 km
  Plane   Strike  Dip  Rake
   NP1      171    47   105
   NP2      330    45    75
  Principal Axes:
   Axis    Value   Plunge  Azimuth
    T   1.64e+21     79     155
    N   0.00e+00     11     341
    P  -1.64e+21      1     251

 Moment Tensor: (dyne-cm)
    Component   Value
       Mxx    -1.36e+20
       Mxy    -5.36e+20
       Mxz    -2.60e+20
       Myy    -1.45e+21
       Myz     1.50e+20
       Mzz     1.58e+21
                                                     
                                                     
                                                     
                                                     
                     ##------------                  
                 -----#----------------              
              ------#######---------------           
             ------###########-------------          
           --------##############------------        
          --------################------------       
         ---------##################-----------      
        ---------####################-----------     
        ---------#####################----------     
       ----------######################----------    
       ----------#######################---------    
       ----------###########   #########---------    
       -----------########## T ##########--------    
          --------##########   ##########-------     
        P ---------######################-------     
          ---------######################------      
          ----------#####################-----       
           ----------####################----        
             ---------##################---          
              ----------################--           
                 ---------#############              
                     --------######                  
                                                     
                                                     
                                                     
 Global CMT Convention Moment Tensor:
      R          T          P
  1.58e+21  -2.60e+20  -1.50e+20 
 -2.60e+20  -1.36e+20   5.36e+20 
 -1.50e+20   5.36e+20  -1.45e+21 


Details of the solution is found at

http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20190110134859/index.html
        

Preferred Solution

The preferred solution from an analysis of the surface-wave spectral amplitude radiation pattern, waveform inversion and first motion observations is

      STK = 330
      DIP = 45
     RAKE = 75
       MW = 3.41
       HS = 2.0

The NDK file is 20190110134859.ndk This is really pushing the process for small events. The Mw is very compatible with the ML(H) ML(Z) and the mLg. The mechanism was tweaked to fit the regional patterns of stress. The manual location shows that the few first motions are compatible with the solution as is the soruce depth.

Moment Tensor Comparison

The following compares this source inversion to others
SLU
SLUFM
 USGS/SLU Moment Tensor Solution
 ENS  2019/01/10 13:48:59:0  45.42  -66.25   5.0 3.8 New Brunswick, Canada
 
 Stations used:
   CN.GGN CN.HKNB CN.MCNB CN.SRNB N4.F64A N4.G65A 
 
 Filtering commands used:
   cut o DIST/3.3 -10 o DIST/3.3 +30
   rtr
   taper w 0.1
   hp c 0.10 n 3 
   lp c 0.50 n 3 
 
 Best Fitting Double Couple
  Mo = 1.64e+21 dyne-cm
  Mw = 3.41 
  Z  = 2 km
  Plane   Strike  Dip  Rake
   NP1      171    47   105
   NP2      330    45    75
  Principal Axes:
   Axis    Value   Plunge  Azimuth
    T   1.64e+21     79     155
    N   0.00e+00     11     341
    P  -1.64e+21      1     251

 Moment Tensor: (dyne-cm)
    Component   Value
       Mxx    -1.36e+20
       Mxy    -5.36e+20
       Mxz    -2.60e+20
       Myy    -1.45e+21
       Myz     1.50e+20
       Mzz     1.58e+21
                                                     
                                                     
                                                     
                                                     
                     ##------------                  
                 -----#----------------              
              ------#######---------------           
             ------###########-------------          
           --------##############------------        
          --------################------------       
         ---------##################-----------      
        ---------####################-----------     
        ---------#####################----------     
       ----------######################----------    
       ----------#######################---------    
       ----------###########   #########---------    
       -----------########## T ##########--------    
          --------##########   ##########-------     
        P ---------######################-------     
          ---------######################------      
          ----------#####################-----       
           ----------####################----        
             ---------##################---          
              ----------################--           
                 ---------#############              
                     --------######                  
                                                     
                                                     
                                                     
 Global CMT Convention Moment Tensor:
      R          T          P
  1.58e+21  -2.60e+20  -1.50e+20 
 -2.60e+20  -1.36e+20   5.36e+20 
 -1.50e+20   5.36e+20  -1.45e+21 


Details of the solution is found at

http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20190110134859/index.html
	


First motions and takeoff angles from an elocate run.

Magnitudes

mLg Magnitude


(a) mLg computed using the IASPEI formula; (b) mLg residuals ; the values used for the trimmed mean are indicated.

ML Magnitude


(a) ML computed using the IASPEI formula for Horizontal components; (b) 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.


(a) ML computed using the IASPEI formula for Vertical components (research); (b) 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.

Context

The next figure presents the focal mechanism for this earthquake (red) in the context of other events (blue) in the SLU Moment Tensor Catalog which are within ± 0.5 degrees of the new event. This comparison is shown in the left panel of the figure. 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).

Waveform Inversion using wvfgrd96

The focal mechanism was determined using broadband seismic waveforms. The location of the event and the and stations used for 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 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 -10 o DIST/3.3 +30
rtr
taper w 0.1
hp c 0.10 n 3 
lp c 0.50 n 3 
The results of this grid search from 0.5 to 19 km depth are as follow:

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96    1.0    35    20   -30   3.33 0.3753
WVFGRD96    2.0   330    45    75   3.41 0.4097
WVFGRD96    3.0   330    45    60   3.40 0.3779
WVFGRD96    4.0    20    60   -55   3.43 0.3293
WVFGRD96    5.0   245    65    75   3.54 0.2930
WVFGRD96    6.0   245    65    75   3.58 0.2696
WVFGRD96    7.0   245    65    65   3.59 0.2470
WVFGRD96    8.0   255    75    80   3.68 0.2377
WVFGRD96    9.0   265    75    80   3.70 0.2385
WVFGRD96   10.0    50    30    20   3.67 0.2426
WVFGRD96   11.0    55    30    25   3.71 0.2538
WVFGRD96   12.0    50    25    15   3.74 0.2606
WVFGRD96   13.0    55    25    25   3.77 0.2701
WVFGRD96   14.0    50    25    15   3.78 0.2757
WVFGRD96   15.0    50    25    15   3.79 0.2807
WVFGRD96   16.0   185    25   -65   3.78 0.2889
WVFGRD96   17.0   200    25   -40   3.79 0.2991
WVFGRD96   18.0   205    25   -30   3.79 0.3040
WVFGRD96   19.0   205    25   -25   3.80 0.3080
WVFGRD96   20.0   210    25   -10   3.83 0.3159
WVFGRD96   21.0   210    25   -15   3.83 0.3202
WVFGRD96   22.0   210    25   -15   3.83 0.3152
WVFGRD96   23.0   190    35   -50   3.81 0.3123
WVFGRD96   24.0   190    35   -50   3.82 0.3227
WVFGRD96   25.0   190    35   -50   3.82 0.3269
WVFGRD96   26.0    20    90    75   3.91 0.3225
WVFGRD96   27.0    20    90    75   3.91 0.3334
WVFGRD96   28.0   195    85   -75   3.88 0.3282
WVFGRD96   29.0    35    25   -30   3.82 0.3313

The best solution is

WVFGRD96    2.0   330    45    75   3.41 0.4097

The mechanism correspond 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 and because the velocity model used in the predictions may not be perfect. 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 -10 o DIST/3.3 +30
rtr
taper w 0.1
hp c 0.10 n 3 
lp c 0.50 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.
Focal mechanism sensitivity at the preferred depth. The red color indicates a very good fit to thewavefroms. 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.

Discussion

Acknowledgements

Thanks also to the many seismic network operators whose dedication make this effort possible: University of Nevada Reno, University of Alaska, University of Washington, Oregon State University, University of Utah, Montana Bureas of Mines, UC Berkely, Caltech, UC San Diego, Saint Louis University, University of Memphis, Lamont Doherty Earth Observatory, the Iris stations and the Transportable Array of EarthScope.

Velocity Model

The CUS.model used for the waveform synthetic seismograms and for the surface wave eigenfunctions and dispersion is as follows:

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 

Quality Control

Here we tabulate the reasons for not using certain digital data sets

The following stations did not have a valid response files:

Last Changed Thu Jan 10 09:27:47 CST 2019