Location
Location ANSS
The ANSS event ID is uw61562126 and the event page is at
https://earthquake.usgs.gov/earthquakes/eventpage/uw61562126/executive.
2019/11/30 01:45:12 42.776 -124.477 16.6 4.53 Oregon
Focal Mechanism
USGS/SLU Moment Tensor Solution
ENS 2019/11/30 01:45:12:0 42.78 -124.48 16.6 4.5 Oregon
Stations used:
BK.BRIC BK.DANT BK.HATC BK.PETY BK.SCOT BK.TRIN CC.CLBH
CC.JRO CC.PRLK CC.SWNB CC.WIFE IU.COR NC.KBO NC.KHBB
NC.KHMB NC.KMR NC.KSXB NC.LDH NC.LMC UO.BEER UO.BUCK
UO.CAVE UO.CHIL UO.DFAZ UO.DING UO.DRAN UO.FHAC UO.JESE
UO.LAIR UO.MARQ UO.MINN UO.NATH UO.PINE UO.ROGE UO.TOOM
UO.VERN UO.WLOO UO.WOOD UO.WYLD UW.BBO UW.BLOW UW.HOOD
UW.IZEE UW.LCCR UW.LEBA UW.TREE
Filtering commands used:
cut o DIST/3.3 -40 o DIST/3.3 +50
rtr
taper w 0.1
hp c 0.03 n 3
lp c 0.10 n 3
Best Fitting Double Couple
Mo = 5.96e+22 dyne-cm
Mw = 4.45
Z = 18 km
Plane Strike Dip Rake
NP1 161 86 115
NP2 260 25 10
Principal Axes:
Axis Value Plunge Azimuth
T 5.96e+22 44 95
N 0.00e+00 25 339
P -5.96e+22 36 229
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.62e+22
Mxy -2.19e+22
Mxz 1.58e+22
Myy 8.24e+21
Myz 5.12e+22
Mzz 7.92e+21
--------------
#####-----------------
########-----#####----------
#######---###############-----
######------###################---
####----------####################--
###------------######################-
###--------------######################-
##---------------#######################
##-----------------#######################
#-------------------########### ########
#-------------------########### T ########
#--------------------########## ########
--------------------####################
-------- ----------###################
------- P -----------#################
------ ------------###############
--------------------##############
-------------------###########
-------------------#########
-----------------#####
--------------
Global CMT Convention Moment Tensor:
R T P
7.92e+21 1.58e+22 -5.12e+22
1.58e+22 -1.62e+22 2.19e+22
-5.12e+22 2.19e+22 8.24e+21
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20191130014512/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 = 260
DIP = 25
RAKE = 10
MW = 4.45
HS = 18.0
The NDK file is 20191130014512.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 |
USGSMWR |
USGS/SLU Moment Tensor Solution
ENS 2019/11/30 01:45:12:0 42.78 -124.48 16.6 4.5 Oregon
Stations used:
BK.BRIC BK.DANT BK.HATC BK.PETY BK.SCOT BK.TRIN CC.CLBH
CC.JRO CC.PRLK CC.SWNB CC.WIFE IU.COR NC.KBO NC.KHBB
NC.KHMB NC.KMR NC.KSXB NC.LDH NC.LMC UO.BEER UO.BUCK
UO.CAVE UO.CHIL UO.DFAZ UO.DING UO.DRAN UO.FHAC UO.JESE
UO.LAIR UO.MARQ UO.MINN UO.NATH UO.PINE UO.ROGE UO.TOOM
UO.VERN UO.WLOO UO.WOOD UO.WYLD UW.BBO UW.BLOW UW.HOOD
UW.IZEE UW.LCCR UW.LEBA UW.TREE
Filtering commands used:
cut o DIST/3.3 -40 o DIST/3.3 +50
rtr
taper w 0.1
hp c 0.03 n 3
lp c 0.10 n 3
Best Fitting Double Couple
Mo = 5.96e+22 dyne-cm
Mw = 4.45
Z = 18 km
Plane Strike Dip Rake
NP1 161 86 115
NP2 260 25 10
Principal Axes:
Axis Value Plunge Azimuth
T 5.96e+22 44 95
N 0.00e+00 25 339
P -5.96e+22 36 229
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.62e+22
Mxy -2.19e+22
Mxz 1.58e+22
Myy 8.24e+21
Myz 5.12e+22
Mzz 7.92e+21
--------------
#####-----------------
########-----#####----------
#######---###############-----
######------###################---
####----------####################--
###------------######################-
###--------------######################-
##---------------#######################
##-----------------#######################
#-------------------########### ########
#-------------------########### T ########
#--------------------########## ########
--------------------####################
-------- ----------###################
------- P -----------#################
------ ------------###############
--------------------##############
-------------------###########
-------------------#########
-----------------#####
--------------
Global CMT Convention Moment Tensor:
R T P
7.92e+21 1.58e+22 -5.12e+22
1.58e+22 -1.62e+22 2.19e+22
-5.12e+22 2.19e+22 8.24e+21
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20191130014512/index.html
|
Regional Moment Tensor (Mwr)
Moment 6.802e+15 N-m
Magnitude 4.49 Mwr
Depth 21.0 km
Percent DC 91%
Half Duration -
Catalog US
Data Source US 3
Contributor US 3
Nodal Planes
Plane Strike Dip Rake
NP1 268Â 25Â 14Â
NP2 165Â 84Â 115Â
Principal Axes
Axis Value Plunge Azimuth
T 6.646e+15 N-m 46Â 100Â
N 0.303e+15 N-m 25Â 342Â
P -6.949e+15 N-m 34Â 234Â
 |
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 +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 1.0 330 45 -90 4.00 0.2674
WVFGRD96 2.0 150 45 -90 4.16 0.3550
WVFGRD96 3.0 325 40 -95 4.18 0.2484
WVFGRD96 4.0 340 85 -65 4.13 0.2333
WVFGRD96 5.0 160 90 65 4.15 0.2933
WVFGRD96 6.0 160 90 65 4.18 0.3493
WVFGRD96 7.0 160 90 65 4.19 0.3960
WVFGRD96 8.0 340 90 -65 4.28 0.4300
WVFGRD96 9.0 160 90 65 4.30 0.4726
WVFGRD96 10.0 160 85 65 4.32 0.5098
WVFGRD96 11.0 335 90 -65 4.34 0.5396
WVFGRD96 12.0 160 85 65 4.36 0.5675
WVFGRD96 13.0 160 85 65 4.38 0.5883
WVFGRD96 14.0 265 25 15 4.39 0.6026
WVFGRD96 15.0 260 25 10 4.41 0.6162
WVFGRD96 16.0 260 25 10 4.43 0.6251
WVFGRD96 17.0 260 25 10 4.44 0.6304
WVFGRD96 18.0 260 25 10 4.45 0.6322
WVFGRD96 19.0 260 25 10 4.47 0.6308
WVFGRD96 20.0 260 25 10 4.48 0.6264
WVFGRD96 21.0 260 25 10 4.50 0.6198
WVFGRD96 22.0 260 25 10 4.51 0.6103
WVFGRD96 23.0 260 25 10 4.52 0.5989
WVFGRD96 24.0 265 25 15 4.53 0.5853
WVFGRD96 25.0 265 25 15 4.54 0.5700
WVFGRD96 26.0 315 40 70 4.56 0.5543
WVFGRD96 27.0 315 40 70 4.57 0.5388
WVFGRD96 28.0 310 40 60 4.58 0.5230
WVFGRD96 29.0 305 40 55 4.58 0.5065
The best solution is
WVFGRD96 18.0 260 25 10 4.45 0.6322
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 +50
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 Thu Apr 25 05:47:12 PM CDT 2024
