Location

Location ANSS

The ANSS event ID is ak02431au8tv and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/ak02431au8tv/executive.

2024/03/06 09:02:05 62.232 -148.200 29.5 4.1 Alaska

Focal Mechanism

USGS/SLU Moment Tensor Solution ENS 2024/03/06 09:02:05:0 62.23 -148.20 29.5 4.1 Alaska Stations used: AK.BAE AK.CUT AK.DIV AK.FID AK.GHO AK.GLI AK.HARP AK.KLU AK.KNK AK.L22K AK.MCK AK.PAX AK.RC01 AK.RND AK.SAW AK.SCM AT.PMR Filtering commands used: cut o DIST/3.5 -40 o DIST/3.5 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.10 n 3 Best Fitting Double Couple Mo = 2.60e+22 dyne-cm Mw = 4.21 Z = 58 km Plane Strike Dip Rake NP1 210 50 -80 NP2 15 41 -102 Principal Axes: Axis Value Plunge Azimuth T 2.60e+22 5 293 N 0.00e+00 8 24 P -2.60e+22 81 173 Moment Tensor: (dyne-cm) Component Value Mxx 3.31e+21 Mxy -9.19e+21 Mxz 4.74e+21 Myy 2.19e+22 Myz -2.40e+21 Mzz -2.52e+22 #############- ##################-### ################-------##### ##############-----------##### ##############--------------###### ############-----------------###### T ###########------------------####### #########--------------------######## ###########----------------------####### ###########-----------------------######## ##########------------------------######## ##########---------- ----------######### #########----------- P ----------######### ########----------- ---------######### ########-----------------------######### ######-----------------------######### #####----------------------######### #####-------------------########## ###------------------######### ###---------------########## ------------########## -----######### Global CMT Convention Moment Tensor: R T P -2.52e+22 4.74e+21 2.40e+21 4.74e+21 3.31e+21 9.19e+21 2.40e+21 9.19e+21 2.19e+22 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20240306090205/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 = 210
      DIP = 50
     RAKE = -80
       MW = 4.21
       HS = 58.0

The NDK file is 20240306090205.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 M_L by application of the respective IASPEI formulae. As a research study, the linear distance term of the IASPEI formula for M_L is adjusted to remove a linear distance trend in residuals to give a regionally defined M_L. The defined M_L 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/3.5 -40 o DIST/3.5 +50
rtr
taper w 0.1
hp c 0.03 n 3 
lp c 0.10 n 3

The results of this grid search are as follow:

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96    2.0    30    45    90   3.42 0.2118
WVFGRD96    4.0   185    35    40   3.46 0.2111
WVFGRD96    6.0     0    45    35   3.47 0.2277
WVFGRD96    8.0     5    45    45   3.58 0.2499
WVFGRD96   10.0     0    50    40   3.61 0.2647
WVFGRD96   12.0     0    65   -45   3.63 0.2663
WVFGRD96   14.0     5    70   -50   3.66 0.2657
WVFGRD96   16.0    70    90   -40   3.67 0.2672
WVFGRD96   18.0   230    50   -55   3.74 0.2873
WVFGRD96   20.0   230    50   -55   3.77 0.3091
WVFGRD96   22.0   230    50   -55   3.81 0.3224
WVFGRD96   24.0    65    65   -30   3.80 0.3293
WVFGRD96   26.0    65    65   -30   3.82 0.3345
WVFGRD96   28.0    65    70   -40   3.84 0.3390
WVFGRD96   30.0    65    65   -35   3.86 0.3543
WVFGRD96   32.0    60    60   -40   3.88 0.3845
WVFGRD96   34.0    60    60   -40   3.90 0.4096
WVFGRD96   36.0    45    50   -65   3.94 0.4327
WVFGRD96   38.0    45    50   -70   3.96 0.4560
WVFGRD96   40.0    40    50   -75   4.08 0.5063
WVFGRD96   42.0   205    40   -95   4.12 0.5148
WVFGRD96   44.0   205    40   -95   4.14 0.5133
WVFGRD96   46.0    30    45   -85   4.15 0.5121
WVFGRD96   48.0   210    45   -85   4.17 0.5177
WVFGRD96   50.0   210    50   -85   4.18 0.5291
WVFGRD96   52.0   210    50   -85   4.19 0.5382
WVFGRD96   54.0   210    50   -80   4.21 0.5434
WVFGRD96   56.0   210    50   -80   4.21 0.5462
WVFGRD96   58.0   210    50   -80   4.21 0.5468
WVFGRD96   60.0   210    50   -80   4.21 0.5447
WVFGRD96   62.0   210    50   -80   4.21 0.5411
WVFGRD96   64.0   210    50   -80   4.21 0.5369
WVFGRD96   66.0   215    55   -70   4.23 0.5372
WVFGRD96   68.0   215    55   -70   4.23 0.5370
WVFGRD96   70.0   215    55   -70   4.23 0.5345
WVFGRD96   72.0   215    55   -70   4.22 0.5308
WVFGRD96   74.0   215    55   -70   4.22 0.5270
WVFGRD96   76.0   220    60   -60   4.25 0.5229
WVFGRD96   78.0   220    60   -60   4.24 0.5196
WVFGRD96   80.0   220    60   -60   4.24 0.5168
WVFGRD96   82.0   220    60   -60   4.24 0.5134
WVFGRD96   84.0   220    65   -55   4.26 0.5097
WVFGRD96   86.0   220    65   -55   4.26 0.5065
WVFGRD96   88.0   220    65   -55   4.26 0.5029
WVFGRD96   90.0   220    65   -55   4.26 0.5002
WVFGRD96   92.0   220    65   -55   4.26 0.4963
WVFGRD96   94.0   220    65   -55   4.26 0.4926
WVFGRD96   96.0   220    70   -55   4.27 0.4897
WVFGRD96   98.0   220    70   -55   4.27 0.4871

The best solution is

WVFGRD96   58.0   210    50   -80   4.21 0.5468

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/3.5 -40 o DIST/3.5 +50
rtr
taper w 0.1
hp c 0.03 n 3 
lp c 0.10 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:

The origin time and epicentral distance are incorrect
The velocity model used for the inversion is incorrect
The velocity model used to define the P-arrival time is not the same as the velocity model used for the waveform inversion (assuming that the initial trace alignment is based on the P arrival time)

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 08:18:52 PM CDT 2024