Location
Location ANSS
The ANSS event ID is nc75411492 and the event page is at
https://earthquake.usgs.gov/earthquakes/eventpage/nc75411492/executive.
2026/08/05 00:25:25 40.028 -123.443 7.5 4.0 California
Focal Mechanism
USGS/SLU Moment Tensor Solution
ENS 2026/08/05 00:25:25.0 40.03 -123.44 7.5 4.0 California
Stations used:
BK.ADAM BK.AUSC BK.BARR BK.BEVN BK.BJES BK.BLAS BK.BONV
BK.BRIC BK.BRIT BK.BTVR BK.DCMP BK.DLIK BK.DMOR BK.ETSL
BK.GALB BK.GASB BK.GCKB BK.GHOP BK.GRPK BK.GTSB BK.GUMB
BK.HALS BK.HATC BK.HAYF BK.HOPS BK.HRCH BK.HULL BK.HUNT
BK.JCC BK.KNEE BK.KRUG BK.LCOW BK.LSIB BK.MNDO BK.MNRC
BK.OAKV BK.ORRS BK.PETL BK.PETY BK.PRDS BK.PWAY BK.PWOD
BK.RBOW BK.SAGE BK.SCOT BK.SHWD BK.SKGS BK.SNCR BK.SUGR
BK.TRIN BK.USAL BK.WEAV BK.WLKR BK.WTWN NC.GDXB NC.GHGB
NC.GRT NC.GSR NC.GSX NC.GTK NC.GWKB NC.KBL NC.KCT NC.KHBB
NC.KHMB NC.KNR NC.KPC NC.KRP NC.KZE NC.LDH NC.LGY NC.LMPB
NC.LTC NC.LWPB NC.NMTB NC.NSM NC.NTYB NC.NWH
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 0.08 n 3
Best Fitting Double Couple
Mo = 1.45e+22 dyne-cm
Mw = 4.04
Z = 13 km
Plane Strike Dip Rake
NP1 143 80 170
NP2 235 80 10
Principal Axes:
Axis Value Plunge Azimuth
T 1.45e+22 14 99
N 0.00e+00 76 280
P -1.45e+22 0 189
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.37e+22
Mxy -4.39e+21
Mxz -5.14e+20
Myy 1.29e+22
Myz 3.38e+21
Mzz 8.58e+20
--------------
----------------------
##--------------------------
####--------------------------
######----------------------------
########----------------------######
##########------------------##########
#############------------###############
##############--------##################
################-----#####################
#################-########################
###############----################## ##
#############-------################# T ##
##########----------################ #
########--------------##################
#####------------------###############
##---------------------#############
------------------------##########
------------------------######
-------------------------###
------ -------------
-- P ---------
Global CMT Convention Moment Tensor:
R T P
8.58e+20 -5.14e+20 -3.38e+21
-5.14e+20 -1.37e+22 4.39e+21
-3.38e+21 4.39e+21 1.29e+22
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20260805002525/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 = 235
DIP = 80
RAKE = 10
MW = 4.04
HS = 13.0
The NDK file is 20260805002525.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 |
UCB |
USGS/SLU Moment Tensor Solution
ENS 2026/08/05 00:25:25.0 40.03 -123.44 7.5 4.0 California
Stations used:
BK.ADAM BK.AUSC BK.BARR BK.BEVN BK.BJES BK.BLAS BK.BONV
BK.BRIC BK.BRIT BK.BTVR BK.DCMP BK.DLIK BK.DMOR BK.ETSL
BK.GALB BK.GASB BK.GCKB BK.GHOP BK.GRPK BK.GTSB BK.GUMB
BK.HALS BK.HATC BK.HAYF BK.HOPS BK.HRCH BK.HULL BK.HUNT
BK.JCC BK.KNEE BK.KRUG BK.LCOW BK.LSIB BK.MNDO BK.MNRC
BK.OAKV BK.ORRS BK.PETL BK.PETY BK.PRDS BK.PWAY BK.PWOD
BK.RBOW BK.SAGE BK.SCOT BK.SHWD BK.SKGS BK.SNCR BK.SUGR
BK.TRIN BK.USAL BK.WEAV BK.WLKR BK.WTWN NC.GDXB NC.GHGB
NC.GRT NC.GSR NC.GSX NC.GTK NC.GWKB NC.KBL NC.KCT NC.KHBB
NC.KHMB NC.KNR NC.KPC NC.KRP NC.KZE NC.LDH NC.LGY NC.LMPB
NC.LTC NC.LWPB NC.NMTB NC.NSM NC.NTYB NC.NWH
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 0.08 n 3
Best Fitting Double Couple
Mo = 1.45e+22 dyne-cm
Mw = 4.04
Z = 13 km
Plane Strike Dip Rake
NP1 143 80 170
NP2 235 80 10
Principal Axes:
Axis Value Plunge Azimuth
T 1.45e+22 14 99
N 0.00e+00 76 280
P -1.45e+22 0 189
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.37e+22
Mxy -4.39e+21
Mxz -5.14e+20
Myy 1.29e+22
Myz 3.38e+21
Mzz 8.58e+20
--------------
----------------------
##--------------------------
####--------------------------
######----------------------------
########----------------------######
##########------------------##########
#############------------###############
##############--------##################
################-----#####################
#################-########################
###############----################## ##
#############-------################# T ##
##########----------################ #
########--------------##################
#####------------------###############
##---------------------#############
------------------------##########
------------------------######
-------------------------###
------ -------------
-- P ---------
Global CMT Convention Moment Tensor:
R T P
8.58e+20 -5.14e+20 -3.38e+21
-5.14e+20 -1.37e+22 4.39e+21
-3.38e+21 4.39e+21 1.29e+22
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20260805002525/index.html
|
Regional Moment Tensor (Mwr)
Moment 1.544e+15 N-m
Magnitude 4.06 Mwr
Depth 17.0 km
Percent DC 83%
Half Duration -
Catalog US
Data Source US
Contributor US
Nodal Planes
Plane Strike Dip Rake
NP1 55 83 -7
NP2 146 83 -173
Principal Axes
Axis Value Plunge Azimuth
T 1.608e+15 0 100
N -0.136e+15 80 193
P -1.472e+15 10 10
|
Moment Tensor (Mw)
Moment 1.218e+15 N-m
Magnitude 3.99 Mw
Depth 8.0 km
Percent DC 74%
Half Duration -
Catalog NC
Data Source NC
Contributor NC
Nodal Planes
Plane Strike Dip Rake
NP1 236 90 7
NP2 146 83 180
Principal Axes
Axis Value Plunge Azimuth
T 1.293e+15 5 101
N -0.168e+15 83 237
P -1.125e+15 5 11
|
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.
Map showing station locations used for computing the ML's. No distinction is made whether the vertical (Z) or horizontal (H) components were used.
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 0.08 n 3
The results of this grid search are as follow:
DEPTH STK DIP RAKE MW FIT
WVFGRD96 1.0 50 90 5 3.55 0.2272
WVFGRD96 2.0 55 90 0 3.68 0.3183
WVFGRD96 3.0 55 90 -10 3.74 0.3507
WVFGRD96 4.0 230 75 -20 3.80 0.3753
WVFGRD96 5.0 235 80 20 3.83 0.4052
WVFGRD96 6.0 55 90 -20 3.87 0.4296
WVFGRD96 7.0 235 80 15 3.90 0.4577
WVFGRD96 8.0 235 80 20 3.94 0.4827
WVFGRD96 9.0 55 90 -15 3.96 0.4951
WVFGRD96 10.0 235 80 15 3.99 0.5119
WVFGRD96 11.0 55 90 -15 4.00 0.5169
WVFGRD96 12.0 235 80 15 4.02 0.5262
WVFGRD96 13.0 235 80 10 4.04 0.5280
WVFGRD96 14.0 235 80 10 4.05 0.5273
WVFGRD96 15.0 55 90 -10 4.06 0.5216
WVFGRD96 16.0 235 85 10 4.07 0.5192
WVFGRD96 17.0 55 90 -10 4.08 0.5102
WVFGRD96 18.0 55 90 -10 4.09 0.5022
WVFGRD96 19.0 235 85 10 4.10 0.4950
WVFGRD96 20.0 235 85 10 4.11 0.4849
WVFGRD96 21.0 55 90 -10 4.11 0.4731
WVFGRD96 22.0 55 90 -10 4.12 0.4619
WVFGRD96 23.0 55 90 -10 4.12 0.4502
WVFGRD96 24.0 55 90 10 4.13 0.4387
WVFGRD96 25.0 55 90 10 4.13 0.4271
WVFGRD96 26.0 55 90 10 4.13 0.4152
WVFGRD96 27.0 235 90 -10 4.14 0.4034
WVFGRD96 28.0 55 90 10 4.14 0.3917
WVFGRD96 29.0 55 90 10 4.14 0.3803
The best solution is
WVFGRD96 13.0 235 80 10 4.04 0.5280
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 0.08 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 Tue Aug 4 21:08:59 CDT 2026
