Location
Location ANSS
The ANSS event ID is ak0158l9sor0 and the event page is at
https://earthquake.usgs.gov/earthquakes/eventpage/ak0158l9sor0/executive.
2015/07/06 00:50:34 62.130 -150.789 70.7 4.8 Alaska
Focal Mechanism
USGS/SLU Moment Tensor Solution
ENS 2015/07/06 00:50:34:0 62.13 -150.79 70.7 4.8 Alaska
Stations used:
AK.BARN AK.BMR AK.BRLK AK.BWN AK.CCB AK.CNP AK.CRQ AK.CTG
AK.CUT AK.DOT AK.EYAK AK.FID AK.GLB AK.GLI AK.HDA AK.HIN
AK.HMT AK.ISLE AK.KLU AK.KNK AK.KTH AK.LOGN AK.MCAR AK.MCK
AK.MDM AK.MLY AK.NEA2 AK.PAX AK.PPD AK.PPLA AK.PWL AK.RC01
AK.RND AK.SAW AK.SCM AK.SCRK AK.SKN AK.SSN AK.SWD AK.TGL
AK.TRF AK.VRDI AK.WAX AK.WRH AT.MENT AT.MID AT.PMR II.KDAK
IM.IL31 IU.COLA TA.I23K TA.K27K TA.L27K TA.M24K TA.N25K
TA.POKR
Filtering commands used:
cut o DIST/3.3 -50 o DIST/3.3 +70
rtr
taper w 0.1
hp c 0.02 n 3
lp c 0.06 n 3
Best Fitting Double Couple
Mo = 2.82e+23 dyne-cm
Mw = 4.90
Z = 76 km
Plane Strike Dip Rake
NP1 337 84 130
NP2 75 40 10
Principal Axes:
Axis Value Plunge Azimuth
T 2.82e+23 38 282
N 0.00e+00 39 152
P -2.82e+23 28 37
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.34e+23
Mxy -1.42e+23
Mxz -6.32e+22
Myy 8.60e+22
Myz -2.03e+23
Mzz 4.82e+22
--------------
####------------------
########--------------------
##########------------- ----
#############------------ P ------
###############----------- -------
#################---------------------
###################---------------------
###### ###########--------------------
####### T ############-------------------#
####### ############------------------##
#######################----------------###
########################--------------####
########################-----------#####
-#######################----------######
--######################------########
----####################--##########
-------#############---###########
----------------------########
---------------------#######
-------------------###
--------------
Global CMT Convention Moment Tensor:
R T P
4.82e+22 -6.32e+22 2.03e+23
-6.32e+22 -1.34e+23 1.42e+23
2.03e+23 1.42e+23 8.60e+22
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20150706005034/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 = 75
DIP = 40
RAKE = 10
MW = 4.90
HS = 76.0
The NDK file is 20150706005034.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 2015/07/06 00:50:34:0 62.13 -150.79 70.7 4.8 Alaska
Stations used:
AK.BARN AK.BMR AK.BRLK AK.BWN AK.CCB AK.CNP AK.CRQ AK.CTG
AK.CUT AK.DOT AK.EYAK AK.FID AK.GLB AK.GLI AK.HDA AK.HIN
AK.HMT AK.ISLE AK.KLU AK.KNK AK.KTH AK.LOGN AK.MCAR AK.MCK
AK.MDM AK.MLY AK.NEA2 AK.PAX AK.PPD AK.PPLA AK.PWL AK.RC01
AK.RND AK.SAW AK.SCM AK.SCRK AK.SKN AK.SSN AK.SWD AK.TGL
AK.TRF AK.VRDI AK.WAX AK.WRH AT.MENT AT.MID AT.PMR II.KDAK
IM.IL31 IU.COLA TA.I23K TA.K27K TA.L27K TA.M24K TA.N25K
TA.POKR
Filtering commands used:
cut o DIST/3.3 -50 o DIST/3.3 +70
rtr
taper w 0.1
hp c 0.02 n 3
lp c 0.06 n 3
Best Fitting Double Couple
Mo = 2.82e+23 dyne-cm
Mw = 4.90
Z = 76 km
Plane Strike Dip Rake
NP1 337 84 130
NP2 75 40 10
Principal Axes:
Axis Value Plunge Azimuth
T 2.82e+23 38 282
N 0.00e+00 39 152
P -2.82e+23 28 37
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.34e+23
Mxy -1.42e+23
Mxz -6.32e+22
Myy 8.60e+22
Myz -2.03e+23
Mzz 4.82e+22
--------------
####------------------
########--------------------
##########------------- ----
#############------------ P ------
###############----------- -------
#################---------------------
###################---------------------
###### ###########--------------------
####### T ############-------------------#
####### ############------------------##
#######################----------------###
########################--------------####
########################-----------#####
-#######################----------######
--######################------########
----####################--##########
-------#############---###########
----------------------########
---------------------#######
-------------------###
--------------
Global CMT Convention Moment Tensor:
R T P
4.82e+22 -6.32e+22 2.03e+23
-6.32e+22 -1.34e+23 1.42e+23
2.03e+23 1.42e+23 8.60e+22
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20150706005034/index.html
|
Regional Moment Tensor (Mwr)
Moment 2.579e+16 N-m
Magnitude 4.87
Depth 65.0 km
Percent DC 90%
Half Duration –
Catalog US (us10002nkt)
Data Source US2
Contributor US2
Nodal Planes
Plane Strike Dip Rake
NP1 338 77 132
NP2 82 44 19
Principal Axes
Axis Value Plunge Azimuth
T 2.511 42 288
N 0.132 41 146
P -2.642 21 38
|
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 +70
rtr
taper w 0.1
hp c 0.02 n 3
lp c 0.06 n 3
The results of this grid search are as follow:
DEPTH STK DIP RAKE MW FIT
WVFGRD96 2.0 65 45 -60 4.10 0.2045
WVFGRD96 4.0 70 75 -5 4.15 0.2333
WVFGRD96 6.0 70 70 0 4.22 0.2600
WVFGRD96 8.0 70 70 5 4.28 0.2873
WVFGRD96 10.0 70 70 5 4.32 0.3042
WVFGRD96 12.0 70 75 10 4.35 0.3141
WVFGRD96 14.0 70 75 15 4.37 0.3222
WVFGRD96 16.0 70 75 10 4.39 0.3306
WVFGRD96 18.0 70 70 10 4.40 0.3410
WVFGRD96 20.0 75 70 15 4.41 0.3550
WVFGRD96 22.0 75 70 15 4.43 0.3702
WVFGRD96 24.0 75 70 15 4.45 0.3846
WVFGRD96 26.0 75 70 15 4.47 0.3992
WVFGRD96 28.0 75 70 15 4.49 0.4141
WVFGRD96 30.0 75 70 15 4.51 0.4289
WVFGRD96 32.0 75 65 15 4.52 0.4450
WVFGRD96 34.0 75 65 15 4.55 0.4627
WVFGRD96 36.0 70 70 10 4.59 0.4823
WVFGRD96 38.0 70 70 10 4.62 0.5064
WVFGRD96 40.0 70 60 10 4.69 0.5187
WVFGRD96 42.0 70 60 10 4.71 0.5316
WVFGRD96 44.0 70 55 5 4.72 0.5475
WVFGRD96 46.0 70 55 5 4.74 0.5651
WVFGRD96 48.0 70 55 10 4.76 0.5828
WVFGRD96 50.0 75 50 10 4.77 0.6039
WVFGRD96 52.0 75 50 15 4.79 0.6230
WVFGRD96 54.0 75 50 15 4.80 0.6433
WVFGRD96 56.0 75 50 15 4.82 0.6609
WVFGRD96 58.0 75 50 15 4.83 0.6772
WVFGRD96 60.0 75 45 15 4.84 0.6940
WVFGRD96 62.0 75 45 15 4.85 0.7090
WVFGRD96 64.0 75 45 15 4.86 0.7215
WVFGRD96 66.0 75 45 15 4.87 0.7314
WVFGRD96 68.0 75 45 15 4.88 0.7392
WVFGRD96 70.0 75 45 15 4.89 0.7446
WVFGRD96 72.0 75 45 15 4.89 0.7480
WVFGRD96 74.0 75 40 10 4.90 0.7509
WVFGRD96 76.0 75 40 10 4.90 0.7520
WVFGRD96 78.0 75 40 10 4.91 0.7517
WVFGRD96 80.0 75 40 10 4.91 0.7496
WVFGRD96 82.0 75 40 10 4.92 0.7455
WVFGRD96 84.0 75 40 10 4.92 0.7404
WVFGRD96 86.0 75 40 10 4.92 0.7334
WVFGRD96 88.0 80 35 10 4.92 0.7263
WVFGRD96 90.0 80 35 10 4.92 0.7180
WVFGRD96 92.0 80 35 10 4.93 0.7108
WVFGRD96 94.0 80 35 10 4.93 0.7024
WVFGRD96 96.0 80 35 10 4.93 0.6925
WVFGRD96 98.0 80 35 10 4.93 0.6815
The best solution is
WVFGRD96 76.0 75 40 10 4.90 0.7520
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 +70
rtr
taper w 0.1
hp c 0.02 n 3
lp c 0.06 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.
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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 Fri Apr 26 07:24:49 PM CDT 2024
