Location

Location ANSS

The ANSS event ID is ak01474j743m and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/ak01474j743m/executive.

2014/06/04 11:58:58 58.980 -136.728 8.1 5.2 Alaska

Focal Mechanism

 USGS/SLU Moment Tensor Solution
 ENS  2014/06/04 11:58:58:0  58.98 -136.73   8.1 5.2 Alaska
 
 Stations used:
   AK.BAL AK.BARN AK.BESE AK.GLB AK.JIS AK.MESA AK.PIN AK.VRDI 
   AK.WAX AK.YAH AT.CRAG AT.MENT AT.SKAG AT.YKU2 CN.DLBC 
   CN.HYT US.WRAK 
 
 Filtering commands used:
   cut a -30 a 180
   rtr
   taper w 0.1
   hp c 0.02 n 3 
   lp c 0.05 n 3 
 
 Best Fitting Double Couple
  Mo = 2.85e+24 dyne-cm
  Mw = 5.57 
  Z  = 15 km
  Plane   Strike  Dip  Rake
   NP1      350    55   120
   NP2      125    45    55
  Principal Axes:
   Axis    Value   Plunge  Azimuth
    T   2.85e+24     65     318
    N   0.00e+00     24     151
    P  -2.85e+24      5      59

 Moment Tensor: (dyne-cm)
    Component   Value
       Mxx    -4.81e+23
       Mxy    -1.49e+24
       Mxz     6.63e+23
       Myy    -1.85e+24
       Myz    -9.47e+23
       Mzz     2.34e+24
                                                     
                                                     
                                                     
                                                     
                     #####---------                  
                 ############----------              
              ################------------           
             ###################-----------          
           ######################----------          
          -#######################--------- P        
         --########################--------   -      
        ---###########   ###########------------     
        ---########### T ###########------------     
       -----##########   ############------------    
       ------########################------------    
       -------#######################------------    
       --------######################------------    
        --------#####################-----------     
        ----------###################-----------     
         -----------#################----------      
          -------------##############---------       
           ----------------#########---------        
             --------------------###---####          
              ---------------------#######           
                 -----------------#####              
                     ------------##                  
                                                     
                                                     
                                                     
 Global CMT Convention Moment Tensor:
      R          T          P
  2.34e+24   6.63e+23   9.47e+23 
  6.63e+23  -4.81e+23   1.49e+24 
  9.47e+23   1.49e+24  -1.85e+24 


Details of the solution is found at

http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20140604115858/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 = 125
      DIP = 45
     RAKE = 55
       MW = 5.57
       HS = 15.0

The NDK file is 20140604115858.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
GCMT
 USGS/SLU Moment Tensor Solution
 ENS  2014/06/04 11:58:58:0  58.98 -136.73   8.1 5.2 Alaska
 
 Stations used:
   AK.BAL AK.BARN AK.BESE AK.GLB AK.JIS AK.MESA AK.PIN AK.VRDI 
   AK.WAX AK.YAH AT.CRAG AT.MENT AT.SKAG AT.YKU2 CN.DLBC 
   CN.HYT US.WRAK 
 
 Filtering commands used:
   cut a -30 a 180
   rtr
   taper w 0.1
   hp c 0.02 n 3 
   lp c 0.05 n 3 
 
 Best Fitting Double Couple
  Mo = 2.85e+24 dyne-cm
  Mw = 5.57 
  Z  = 15 km
  Plane   Strike  Dip  Rake
   NP1      350    55   120
   NP2      125    45    55
  Principal Axes:
   Axis    Value   Plunge  Azimuth
    T   2.85e+24     65     318
    N   0.00e+00     24     151
    P  -2.85e+24      5      59

 Moment Tensor: (dyne-cm)
    Component   Value
       Mxx    -4.81e+23
       Mxy    -1.49e+24
       Mxz     6.63e+23
       Myy    -1.85e+24
       Myz    -9.47e+23
       Mzz     2.34e+24
                                                     
                                                     
                                                     
                                                     
                     #####---------                  
                 ############----------              
              ################------------           
             ###################-----------          
           ######################----------          
          -#######################--------- P        
         --########################--------   -      
        ---###########   ###########------------     
        ---########### T ###########------------     
       -----##########   ############------------    
       ------########################------------    
       -------#######################------------    
       --------######################------------    
        --------#####################-----------     
        ----------###################-----------     
         -----------#################----------      
          -------------##############---------       
           ----------------#########---------        
             --------------------###---####          
              ---------------------#######           
                 -----------------#####              
                     ------------##                  
                                                     
                                                     
                                                     
 Global CMT Convention Moment Tensor:
      R          T          P
  2.34e+24   6.63e+23   9.47e+23 
  6.63e+23  -4.81e+23   1.49e+24 
  9.47e+23   1.49e+24  -1.85e+24 


Details of the solution is found at

http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20140604115858/index.html
	
Body-wave Moment Tensor (Mwb)

Moment magnitude derived from a moment tensor 
inversion of long-period (~10 - 100 s) body-waves 
(P-, SH- ) at teleseismic distances (~30 to ~90 degrees).

Moment       2.99e+17 N-m
Magnitude    5.6
Percent DC   95%
Depth        11.0 km
Updated      2014-06-04 12:59:37 UTC
Author       us
Catalog      us
Contributor  us
Code         us_c000rauc_mwb

Principal Axes
Axis	Value	Plunge	Azimuth
T	3.028	69 	303 
N	-0.070	18 	156 
P	-2.958	10 	63 
Nodal Planes
Plane	Strike	Dip	Rake
NP1	348 	58 	111 
NP2	132 	38 	61 



        
SOUTHEASTERN ALASKA, MW=5.7

Howard Koss
Goran Ekstrom

CENTROID-MOMENT-TENSOR  SOLUTION
GCMT EVENT:     C201406041158A
DATA: II IU LD CU MN G  IC GE DK
 KP
L.P.BODY WAVES:155S, 301C, T= 40
MANTLE WAVES:   98S, 115C, T=125
SURFACE WAVES: 167S, 375C, T= 50
TIMESTAMP:      Q-20140604135850
CENTROID LOCATION:
ORIGIN TIME:      11:59:02.4 0.1
LAT:59.08N 0.01;LON:136.71W 0.01
DEP: 17.5  0.3;TRIANG HDUR:  1.8
MOMENT TENSOR: SCALE 10**24 D-CM
RR= 4.220 0.046; TT=-0.600 0.039
PP=-3.620 0.039; RT= 2.140 0.109
RP= 0.495 0.098; TP= 2.550 0.031
PRINCIPAL AXES:
1.(T) VAL=  5.263;PLG=64;AZM=338
2.(N)      -0.143;    25;    147
3.(P)      -5.120;     4;    239
BEST DBLE.COUPLE:M0= 5.19*10**24
NP1: STRIKE=354;DIP=46;SLIP= 126
NP2: STRIKE=127;DIP=54;SLIP=  58

            #####------
        ############-------
      ################-------
    ###################--------
   -####################--------
  ---#########   ########--------
  ---######### T ########--------
 -----########   #########--------
 ------###################--------
 -------##################--------
 ---------################--------
  ----------##############-------
     ---------############-------
   P ------------########-------
     -----------------##------#
      ------------------#####
        --------------#####
            --------###
        

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 a -30 a 180
rtr
taper w 0.1
hp c 0.02 n 3 
lp c 0.05 n 3 
The results of this grid search are as follow:

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96    1.0    90    65   -25   5.26 0.3496
WVFGRD96    2.0    90    65   -30   5.34 0.3967
WVFGRD96    3.0   270    65   -30   5.38 0.3944
WVFGRD96    4.0   270    45   -20   5.43 0.4040
WVFGRD96    5.0   275    45   -15   5.43 0.4282
WVFGRD96    6.0   275    50   -10   5.44 0.4485
WVFGRD96    7.0   275    50   -10   5.45 0.4646
WVFGRD96    8.0   275    45   -10   5.49 0.4801
WVFGRD96    9.0   105    45    20   5.51 0.5084
WVFGRD96   10.0   110    45    35   5.54 0.5454
WVFGRD96   11.0   115    45    45   5.56 0.5804
WVFGRD96   12.0   120    45    50   5.57 0.6073
WVFGRD96   13.0   120    45    50   5.57 0.6248
WVFGRD96   14.0   125    45    55   5.57 0.6341
WVFGRD96   15.0   125    45    55   5.57 0.6378
WVFGRD96   16.0   115    50    45   5.58 0.6374
WVFGRD96   17.0   115    50    40   5.57 0.6343
WVFGRD96   18.0   115    50    40   5.57 0.6287
WVFGRD96   19.0   115    50    40   5.58 0.6208
WVFGRD96   20.0   110    55    30   5.58 0.6126
WVFGRD96   21.0   110    55    30   5.59 0.6047
WVFGRD96   22.0   110    55    30   5.59 0.5941
WVFGRD96   23.0   110    55    30   5.60 0.5830
WVFGRD96   24.0   110    55    25   5.60 0.5713
WVFGRD96   25.0   110    55    25   5.60 0.5596
WVFGRD96   26.0   110    55    25   5.61 0.5474
WVFGRD96   27.0   110    55    25   5.61 0.5347
WVFGRD96   28.0   110    55    25   5.61 0.5219
WVFGRD96   29.0   110    55    25   5.62 0.5091

The best solution is

WVFGRD96   15.0   125    45    55   5.57 0.6378

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 a -30 a 180
rtr
taper w 0.1
hp c 0.02 n 3 
lp c 0.05 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 Fri Apr 26 07:15:45 PM CDT 2024