Location
Location ANSS
The ANSS event ID is ak0176w3wvpo and the event page is at
https://earthquake.usgs.gov/earthquakes/eventpage/ak0176w3wvpo/executive.
2017/05/30 02:18:45 60.834 -151.815 81.2 5.2 Alaska
Focal Mechanism
USGS/SLU Moment Tensor Solution
ENS 2017/05/30 02:18:45:0 60.83 -151.82 81.2 5.2 Alaska
Stations used:
AK.BRLK AK.CAPN AK.CAST AK.CNP AK.CUT AK.FIRE AK.GHO AK.HOM
AK.RC01 AK.SAW AK.SSN AK.SWD AT.PMR AT.SVW2 AV.ILSW TA.L19K
TA.M19K TA.M20K TA.M22K TA.N18K TA.N19K TA.O18K TA.O22K
TA.P18K TA.Q19K
Filtering commands used:
cut o DIST/3.3 -50 o DIST/3.3 +40
rtr
taper w 0.1
hp c 0.03 n 3
lp c 0.10 n 3
Best Fitting Double Couple
Mo = 9.44e+23 dyne-cm
Mw = 5.25
Z = 96 km
Plane Strike Dip Rake
NP1 185 75 -85
NP2 346 16 -108
Principal Axes:
Axis Value Plunge Azimuth
T 9.44e+23 30 271
N 0.00e+00 5 4
P -9.44e+23 60 102
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.02e+22
Mxy 3.74e+22
Mxz 9.22e+22
Myy 4.80e+23
Myz -8.10e+23
Mzz -4.70e+23
########--####
###########-------####
#############-----------####
##############-------------###
###############---------------####
################-----------------###
################-------------------###
#################--------------------###
#################--------------------###
##### #########----------------------###
##### T #########---------- ---------###
##### #########---------- P ---------###
#################---------- ---------###
################---------------------###
################---------------------###
###############--------------------###
##############--------------------##
#############-------------------##
###########-----------------##
###########---------------##
########-------------#
#####---------
Global CMT Convention Moment Tensor:
R T P
-4.70e+23 9.22e+22 8.10e+23
9.22e+22 -1.02e+22 -3.74e+22
8.10e+23 -3.74e+22 4.80e+23
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20170530021845/index.html
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Preferred Solution
The preferred solution from an analysis of the surface-wave spectral amplitude radiation pattern, waveform inversion or first motion observations is
STK = 185
DIP = 75
RAKE = -85
MW = 5.25
HS = 96.0
The NDK file is 20170530021845.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 |
USGS/SLU Moment Tensor Solution
ENS 2017/05/30 02:18:45:0 60.83 -151.82 81.2 5.2 Alaska
Stations used:
AK.BRLK AK.CAPN AK.CAST AK.CNP AK.CUT AK.FIRE AK.GHO AK.HOM
AK.RC01 AK.SAW AK.SSN AK.SWD AT.PMR AT.SVW2 AV.ILSW TA.L19K
TA.M19K TA.M20K TA.M22K TA.N18K TA.N19K TA.O18K TA.O22K
TA.P18K TA.Q19K
Filtering commands used:
cut o DIST/3.3 -50 o DIST/3.3 +40
rtr
taper w 0.1
hp c 0.03 n 3
lp c 0.10 n 3
Best Fitting Double Couple
Mo = 9.44e+23 dyne-cm
Mw = 5.25
Z = 96 km
Plane Strike Dip Rake
NP1 185 75 -85
NP2 346 16 -108
Principal Axes:
Axis Value Plunge Azimuth
T 9.44e+23 30 271
N 0.00e+00 5 4
P -9.44e+23 60 102
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.02e+22
Mxy 3.74e+22
Mxz 9.22e+22
Myy 4.80e+23
Myz -8.10e+23
Mzz -4.70e+23
########--####
###########-------####
#############-----------####
##############-------------###
###############---------------####
################-----------------###
################-------------------###
#################--------------------###
#################--------------------###
##### #########----------------------###
##### T #########---------- ---------###
##### #########---------- P ---------###
#################---------- ---------###
################---------------------###
################---------------------###
###############--------------------###
##############--------------------##
#############-------------------##
###########-----------------##
###########---------------##
########-------------#
#####---------
Global CMT Convention Moment Tensor:
R T P
-4.70e+23 9.22e+22 8.10e+23
9.22e+22 -1.02e+22 -3.74e+22
8.10e+23 -3.74e+22 4.80e+23
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20170530021845/index.html
|
Regional Moment Tensor (Mwr)
Moment 8.549e+16 N-m
Magnitude 5.2 Mwr
Depth 91.0 km
Percent DC 80 %
Half Duration –
Catalog US
Data Source US3
Contributor US3
Nodal Planes
Plane Strike Dip Rake
NP1 342 21 -112
NP2 186 70 -82
Principal Axes
Axis Value Plunge Azimuth
T 8.071e+16 N-m 25 269
N 0.888e+16 N-m 8 3
P -8.959e+16 N-m 64 109
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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.
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Location of broadband stations used for waveform inversion
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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 -50 o DIST/3.3 +40
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 5 55 95 4.33 0.1208
WVFGRD96 4.0 300 55 -50 4.36 0.1269
WVFGRD96 6.0 265 35 -40 4.44 0.1631
WVFGRD96 8.0 265 35 -40 4.53 0.1810
WVFGRD96 10.0 300 50 -45 4.55 0.1983
WVFGRD96 12.0 300 50 -40 4.58 0.2049
WVFGRD96 14.0 305 55 -40 4.60 0.2058
WVFGRD96 16.0 310 60 -40 4.62 0.2037
WVFGRD96 18.0 310 60 -40 4.65 0.1986
WVFGRD96 20.0 315 65 -35 4.67 0.1975
WVFGRD96 22.0 320 70 -35 4.69 0.1952
WVFGRD96 24.0 325 75 -40 4.71 0.1943
WVFGRD96 26.0 335 85 -45 4.73 0.1954
WVFGRD96 28.0 190 85 60 4.78 0.2011
WVFGRD96 30.0 190 85 60 4.81 0.2025
WVFGRD96 32.0 5 90 -60 4.82 0.1987
WVFGRD96 34.0 25 80 -70 4.83 0.1995
WVFGRD96 36.0 30 75 -65 4.83 0.2049
WVFGRD96 38.0 30 70 -65 4.84 0.2171
WVFGRD96 40.0 30 65 -65 4.97 0.2580
WVFGRD96 42.0 25 55 -70 5.00 0.3001
WVFGRD96 44.0 25 50 -70 5.04 0.3404
WVFGRD96 46.0 20 45 -75 5.07 0.3704
WVFGRD96 48.0 25 45 -70 5.09 0.3840
WVFGRD96 50.0 20 40 -75 5.11 0.3967
WVFGRD96 52.0 15 35 -80 5.13 0.4096
WVFGRD96 54.0 200 55 -80 5.13 0.4270
WVFGRD96 56.0 185 55 -90 5.14 0.4420
WVFGRD96 58.0 185 55 -90 5.15 0.4573
WVFGRD96 60.0 185 60 -90 5.17 0.4747
WVFGRD96 62.0 185 60 -90 5.17 0.4892
WVFGRD96 64.0 185 60 -90 5.18 0.5010
WVFGRD96 66.0 5 30 -90 5.18 0.5139
WVFGRD96 68.0 185 65 -90 5.19 0.5216
WVFGRD96 70.0 0 25 -95 5.20 0.5319
WVFGRD96 72.0 185 65 -90 5.20 0.5394
WVFGRD96 74.0 0 25 -95 5.20 0.5452
WVFGRD96 76.0 185 65 -90 5.20 0.5507
WVFGRD96 78.0 185 65 -90 5.20 0.5536
WVFGRD96 80.0 185 65 -90 5.20 0.5575
WVFGRD96 82.0 185 70 -85 5.22 0.5592
WVFGRD96 84.0 -5 20 -100 5.22 0.5660
WVFGRD96 86.0 -5 20 -100 5.22 0.5669
WVFGRD96 88.0 -10 20 -105 5.23 0.5711
WVFGRD96 90.0 -10 20 -105 5.23 0.5711
WVFGRD96 92.0 185 70 -85 5.23 0.5730
WVFGRD96 94.0 -15 20 -110 5.23 0.5743
WVFGRD96 96.0 185 75 -85 5.25 0.5751
WVFGRD96 98.0 -15 20 -110 5.23 0.5749
WVFGRD96 100.0 -10 15 -100 5.25 0.5732
WVFGRD96 102.0 -10 15 -100 5.25 0.5736
WVFGRD96 104.0 -15 15 -105 5.26 0.5706
WVFGRD96 106.0 -15 15 -105 5.26 0.5717
WVFGRD96 108.0 -15 15 -105 5.26 0.5695
WVFGRD96 110.0 -20 15 -110 5.26 0.5668
WVFGRD96 112.0 185 75 -80 5.25 0.5651
WVFGRD96 114.0 185 75 -80 5.25 0.5607
WVFGRD96 116.0 185 75 -80 5.25 0.5573
WVFGRD96 118.0 185 75 -80 5.25 0.5531
The best solution is
WVFGRD96 96.0 185 75 -85 5.25 0.5751
The mechanism corresponding to the best fit is
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Figure 1. Waveform inversion focal mechanism
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The best fit as a function of depth is given in the following figure:
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Figure 2. Depth sensitivity for waveform mechanism
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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 -50 o DIST/3.3 +40
rtr
taper w 0.1
hp c 0.03 n 3
lp c 0.10 n 3
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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.
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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.
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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 Sat Apr 27 01:26:37 PM CDT 2024
