Location
Location ANSS
The ANSS event ID is ak0194n7hhj6 and the event page is at
https://earthquake.usgs.gov/earthquakes/eventpage/ak0194n7hhj6/executive.
2019/04/11 10:42:46 64.735 -149.189 19.9 4.5 Alaska
Focal Mechanism
USGS/SLU Moment Tensor Solution
ENS 2019/04/11 10:42:46:0 64.74 -149.19 19.9 4.5 Alaska
Stations used:
AK.BPAW AK.BWN AK.CAST AK.CCB AK.CHUM AK.COLD AK.CUT AK.DOT
AK.GCSA AK.GHO AK.HDA AK.KLU AK.KNK AK.KTH AK.MCK AK.NEA2
AK.PAX AK.PPLA AK.RIDG AK.RND AK.SAW AK.SCM AK.SCRK AK.SKN
AK.SSN AK.TRF AK.WRH AT.MENT AT.PMR AT.TTA AV.STLK AV.WACK
AV.WAZA IU.COLA TA.E23K TA.E24K TA.F21K TA.F22K TA.F24K
TA.F25K TA.G21K TA.G22K TA.G23K TA.G24K TA.G26K TA.H19K
TA.H20K TA.H21K TA.H22K TA.H23K TA.H24K TA.H25L TA.H27K
TA.I21K TA.I23K TA.J18K TA.J19K TA.J20K TA.J25K TA.J26L
TA.K20K TA.K27K TA.L19K TA.L26K TA.M20K TA.M22K TA.M23K
TA.POKR XV.F4TN XV.F5MN XV.F8KN XV.FAPT XV.FNN1 XV.FNN2
Filtering commands used:
cut o DIST/3.3 -40 o DIST/3.3 +60
rtr
taper w 0.1
hp c 0.03 n 3
lp c 0.08 n 3
Best Fitting Double Couple
Mo = 2.79e+22 dyne-cm
Mw = 4.23
Z = 15 km
Plane Strike Dip Rake
NP1 299 81 -155
NP2 205 65 -10
Principal Axes:
Axis Value Plunge Azimuth
T 2.79e+22 11 70
N 0.00e+00 63 318
P -2.79e+22 24 165
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.84e+22
Mxy 1.46e+22
Mxz 1.18e+22
Myy 2.21e+22
Myz 2.08e+21
Mzz -3.71e+21
--------------
-----------------#####
------------------##########
-----------------#############
-----------------#################
-----------------###################
#######---------###################
############----#################### T #
###############-#################### #
###############------#####################
##############----------##################
##############-------------###############
#############-----------------############
############--------------------########
###########-----------------------######
##########-------------------------###
#########---------------------------
#######---------------------------
#####------------- ---------
#####------------ P --------
##------------ -----
--------------
Global CMT Convention Moment Tensor:
R T P
-3.71e+21 1.18e+22 -2.08e+21
1.18e+22 -1.84e+22 -1.46e+22
-2.08e+21 -1.46e+22 2.21e+22
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20190411104246/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 = 205
DIP = 65
RAKE = -10
MW = 4.23
HS = 15.0
The NDK file is 20190411104246.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 |
USGSW |
USGS/SLU Moment Tensor Solution
ENS 2019/04/11 10:42:46:0 64.74 -149.19 19.9 4.5 Alaska
Stations used:
AK.BPAW AK.BWN AK.CAST AK.CCB AK.CHUM AK.COLD AK.CUT AK.DOT
AK.GCSA AK.GHO AK.HDA AK.KLU AK.KNK AK.KTH AK.MCK AK.NEA2
AK.PAX AK.PPLA AK.RIDG AK.RND AK.SAW AK.SCM AK.SCRK AK.SKN
AK.SSN AK.TRF AK.WRH AT.MENT AT.PMR AT.TTA AV.STLK AV.WACK
AV.WAZA IU.COLA TA.E23K TA.E24K TA.F21K TA.F22K TA.F24K
TA.F25K TA.G21K TA.G22K TA.G23K TA.G24K TA.G26K TA.H19K
TA.H20K TA.H21K TA.H22K TA.H23K TA.H24K TA.H25L TA.H27K
TA.I21K TA.I23K TA.J18K TA.J19K TA.J20K TA.J25K TA.J26L
TA.K20K TA.K27K TA.L19K TA.L26K TA.M20K TA.M22K TA.M23K
TA.POKR XV.F4TN XV.F5MN XV.F8KN XV.FAPT XV.FNN1 XV.FNN2
Filtering commands used:
cut o DIST/3.3 -40 o DIST/3.3 +60
rtr
taper w 0.1
hp c 0.03 n 3
lp c 0.08 n 3
Best Fitting Double Couple
Mo = 2.79e+22 dyne-cm
Mw = 4.23
Z = 15 km
Plane Strike Dip Rake
NP1 299 81 -155
NP2 205 65 -10
Principal Axes:
Axis Value Plunge Azimuth
T 2.79e+22 11 70
N 0.00e+00 63 318
P -2.79e+22 24 165
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.84e+22
Mxy 1.46e+22
Mxz 1.18e+22
Myy 2.21e+22
Myz 2.08e+21
Mzz -3.71e+21
--------------
-----------------#####
------------------##########
-----------------#############
-----------------#################
-----------------###################
#######---------###################
############----#################### T #
###############-#################### #
###############------#####################
##############----------##################
##############-------------###############
#############-----------------############
############--------------------########
###########-----------------------######
##########-------------------------###
#########---------------------------
#######---------------------------
#####------------- ---------
#####------------ P --------
##------------ -----
--------------
Global CMT Convention Moment Tensor:
R T P
-3.71e+21 1.18e+22 -2.08e+21
1.18e+22 -1.84e+22 -1.46e+22
-2.08e+21 -1.46e+22 2.21e+22
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20190411104246/index.html
|
W-phase Moment Tensor (Mww)
Moment 5.792e+15 N-m
Magnitude 4.44 Mww
Depth 15.5 km
Percent DC 27%
Half Duration 0.38 s
Catalog US
Data Source US 2
Contributor US 2
Nodal Planes
Plane Strike Dip Rake
NP1 184 54 -15
NP2 283 78 -143
Principal Axes
Axis Value Plunge Azimuth
T 4.184e+15 N-m 16 49
N 2.426e+15 N-m 51 298
P -6.610e+15 N-m 34 150
|
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.
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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 -40 o DIST/3.3 +60
rtr
taper w 0.1
hp c 0.03 n 3
lp c 0.08 n 3
The results of this grid search are as follow:
DEPTH STK DIP RAKE MW FIT
WVFGRD96 1.0 220 70 10 3.75 0.2412
WVFGRD96 2.0 220 65 10 3.88 0.3144
WVFGRD96 3.0 210 50 -5 3.96 0.3548
WVFGRD96 4.0 205 50 -10 4.00 0.4006
WVFGRD96 5.0 205 55 -10 4.02 0.4375
WVFGRD96 6.0 205 55 -10 4.04 0.4680
WVFGRD96 7.0 205 60 -10 4.06 0.4934
WVFGRD96 8.0 205 55 -10 4.11 0.5151
WVFGRD96 9.0 200 60 -20 4.14 0.5356
WVFGRD96 10.0 200 60 -20 4.16 0.5514
WVFGRD96 11.0 200 60 -15 4.17 0.5642
WVFGRD96 12.0 205 65 -10 4.19 0.5738
WVFGRD96 13.0 205 65 -10 4.20 0.5810
WVFGRD96 14.0 205 65 -10 4.22 0.5844
WVFGRD96 15.0 205 65 -10 4.23 0.5866
WVFGRD96 16.0 205 65 -10 4.24 0.5858
WVFGRD96 17.0 205 65 -10 4.25 0.5834
WVFGRD96 18.0 205 65 -5 4.27 0.5802
WVFGRD96 19.0 205 65 -5 4.28 0.5744
WVFGRD96 20.0 205 65 -5 4.29 0.5674
WVFGRD96 21.0 205 65 -5 4.30 0.5587
WVFGRD96 22.0 205 65 -5 4.31 0.5489
WVFGRD96 23.0 205 65 -5 4.32 0.5380
WVFGRD96 24.0 205 65 -5 4.32 0.5262
WVFGRD96 25.0 205 65 -5 4.33 0.5138
WVFGRD96 26.0 205 60 -5 4.33 0.5015
WVFGRD96 27.0 205 60 -5 4.34 0.4891
WVFGRD96 28.0 205 65 -5 4.35 0.4769
WVFGRD96 29.0 205 65 -5 4.36 0.4644
The best solution is
WVFGRD96 15.0 205 65 -10 4.23 0.5866
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 -40 o DIST/3.3 +60
rtr
taper w 0.1
hp c 0.03 n 3
lp c 0.08 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 Thu Apr 25 11:06:38 AM CDT 2024
