Location
Location ANSS
2017/07/06 15:27:57 46.900 -112.493 26.2 3.7 Montana
Focal Mechanism
USGS/SLU Moment Tensor Solution
ENS 2017/07/06 15:27:57:0 46.90 -112.49 26.2 3.7 Montana
Stations used:
IW.DLMT IW.FXWY IW.PLID IW.REDW IW.SNOW RV.MKRVA US.BMO
US.BOZ US.EGMT US.HLID US.MSO US.NEW US.RLMT UW.TUCA WY.YHL
WY.YMP WY.YMR WY.YNR
Filtering commands used:
cut o DIST/3.3 -30 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 = 5.13e+21 dyne-cm
Mw = 3.74
Z = 20 km
Plane Strike Dip Rake
NP1 195 65 -30
NP2 299 63 -152
Principal Axes:
Axis Value Plunge Azimuth
T 5.13e+21 1 247
N 0.00e+00 52 339
P -5.13e+21 38 156
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.88e+21
Mxy 2.99e+21
Mxz 2.24e+21
Myy 3.85e+21
Myz -1.11e+21
Mzz -1.96e+21
-----------###
-------------#########
---------------#############
--------------################
---------------###################
-#########-----#####################
###############--#####################
###############-------##################
###############-----------##############
###############--------------#############
###############-----------------##########
##############--------------------########
##############---------------------#######
#############-----------------------####
#########-------------------------###
T #########--------------------------#
#########------------ -----------
#########------------ P ----------
########----------- --------
#######---------------------
#####-----------------
#-------------
Global CMT Convention Moment Tensor:
R T P
-1.96e+21 2.24e+21 1.11e+21
2.24e+21 -1.88e+21 -2.99e+21
1.11e+21 -2.99e+21 3.85e+21
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20170706152757/index.html
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Preferred Solution
The preferred solution from an analysis of the surface-wave spectral amplitude radiation pattern, waveform inversion and first motion observations is
STK = 195
DIP = 65
RAKE = -30
MW = 3.74
HS = 20.0
The NDK file is 20170706152757.ndk
The waveform inversion is preferred.
Moment Tensor Comparison
The following compares this source inversion to others
| SLU |
USGSMWR |
USGS/SLU Moment Tensor Solution
ENS 2017/07/06 15:27:57:0 46.90 -112.49 26.2 3.7 Montana
Stations used:
IW.DLMT IW.FXWY IW.PLID IW.REDW IW.SNOW RV.MKRVA US.BMO
US.BOZ US.EGMT US.HLID US.MSO US.NEW US.RLMT UW.TUCA WY.YHL
WY.YMP WY.YMR WY.YNR
Filtering commands used:
cut o DIST/3.3 -30 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 = 5.13e+21 dyne-cm
Mw = 3.74
Z = 20 km
Plane Strike Dip Rake
NP1 195 65 -30
NP2 299 63 -152
Principal Axes:
Axis Value Plunge Azimuth
T 5.13e+21 1 247
N 0.00e+00 52 339
P -5.13e+21 38 156
Moment Tensor: (dyne-cm)
Component Value
Mxx -1.88e+21
Mxy 2.99e+21
Mxz 2.24e+21
Myy 3.85e+21
Myz -1.11e+21
Mzz -1.96e+21
-----------###
-------------#########
---------------#############
--------------################
---------------###################
-#########-----#####################
###############--#####################
###############-------##################
###############-----------##############
###############--------------#############
###############-----------------##########
##############--------------------########
##############---------------------#######
#############-----------------------####
#########-------------------------###
T #########--------------------------#
#########------------ -----------
#########------------ P ----------
########----------- --------
#######---------------------
#####-----------------
#-------------
Global CMT Convention Moment Tensor:
R T P
-1.96e+21 2.24e+21 1.11e+21
2.24e+21 -1.88e+21 -2.99e+21
1.11e+21 -2.99e+21 3.85e+21
Details of the solution is found at
http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20170706152757/index.html
|
Regional Moment Tensor (Mwr)
Moment 4.572e+14 N-m
Magnitude 3.7 Mwr
Depth 23.0 km
Percent DC 98 %
Half Duration –
Catalog US
Data Source US1
Contributor US1
Nodal Planes
Plane Strike Dip Rake
NP1 296 71 -174
NP2 204 84 -19
Principal Axes
Axis Value Plunge Azimuth
T 4.546e+14 N-m 9 251
N 0.050e+14 N-m 70 8
P -4.597e+14 N-m 18 158
|
Magnitudes
ML Magnitude
(a) ML computed using the IASPEI formula for Horizontal components; (b) 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.
(a) ML computed using the IASPEI formula for Vertical components (research); (b) 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.
Context
The next figure presents the focal mechanism for this earthquake (red) in the context of other events (blue) in the SLU Moment Tensor Catalog which are within ± 0.5 degrees of the new event. This comparison is shown in the left panel of the figure. 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).
Waveform Inversion using wvfgrd96
The focal mechanism was determined using broadband seismic waveforms. The location of the event and the
and stations used for 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 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 -30 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 from 0.5 to 19 km depth are as follow:
DEPTH STK DIP RAKE MW FIT
WVFGRD96 1.0 140 45 90 3.47 0.4113
WVFGRD96 2.0 215 50 85 3.53 0.4071
WVFGRD96 3.0 30 60 30 3.51 0.3974
WVFGRD96 4.0 190 80 -45 3.49 0.4087
WVFGRD96 5.0 195 85 -45 3.49 0.4325
WVFGRD96 6.0 190 80 -45 3.50 0.4598
WVFGRD96 7.0 190 80 -45 3.51 0.4860
WVFGRD96 8.0 190 75 -40 3.53 0.5096
WVFGRD96 9.0 190 75 -40 3.54 0.5326
WVFGRD96 10.0 185 70 -45 3.57 0.5514
WVFGRD96 11.0 190 70 -40 3.59 0.5711
WVFGRD96 12.0 190 70 -40 3.61 0.5871
WVFGRD96 13.0 190 65 -35 3.63 0.6032
WVFGRD96 14.0 190 65 -35 3.64 0.6197
WVFGRD96 15.0 195 65 -30 3.66 0.6327
WVFGRD96 16.0 195 65 -30 3.67 0.6420
WVFGRD96 17.0 195 65 -30 3.69 0.6481
WVFGRD96 18.0 195 65 -30 3.70 0.6507
WVFGRD96 19.0 195 65 -30 3.71 0.6499
WVFGRD96 20.0 195 65 -30 3.74 0.6532
WVFGRD96 21.0 195 65 -30 3.75 0.6489
WVFGRD96 22.0 195 65 -30 3.76 0.6427
WVFGRD96 23.0 195 65 -30 3.77 0.6343
WVFGRD96 24.0 195 65 -30 3.78 0.6227
WVFGRD96 25.0 195 65 -30 3.78 0.6080
WVFGRD96 26.0 195 65 -30 3.79 0.5917
WVFGRD96 27.0 195 65 -30 3.79 0.5738
WVFGRD96 28.0 195 65 -30 3.80 0.5539
WVFGRD96 29.0 195 60 -30 3.81 0.5319
The best solution is
WVFGRD96 20.0 195 65 -30 3.74 0.6532
The mechanism correspond 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 and because the velocity model used in the predictions may not be perfect.
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 -30 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.
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Focal mechanism sensitivity at the preferred depth. The red color indicates a very good fit to thewavefroms.
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.
Discussion
Acknowledgements
Thanks also to the many seismic network operators whose dedication make this effort possible: University of Nevada Reno, University of Alaska, University of Washington, Oregon State University, University of Utah, Montana Bureas of Mines, UC Berkely, Caltech, UC San Diego, Saint Louis University, University of Memphis, Lamont Doherty Earth Observatory, the Iris stations and the Transportable Array of EarthScope.
Velocity Model
The CUS.model used for the waveform synthetic seismograms and for the surface wave eigenfunctions and dispersion is as follows:
MODEL.01
CUS Model with Q from simple gamma values
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
1.0000 5.0000 2.8900 2.5000 0.172E-02 0.387E-02 0.00 0.00 1.00 1.00
9.0000 6.1000 3.5200 2.7300 0.160E-02 0.363E-02 0.00 0.00 1.00 1.00
10.0000 6.4000 3.7000 2.8200 0.149E-02 0.336E-02 0.00 0.00 1.00 1.00
20.0000 6.7000 3.8700 2.9020 0.000E-04 0.000E-04 0.00 0.00 1.00 1.00
0.0000 8.1500 4.7000 3.3640 0.194E-02 0.431E-02 0.00 0.00 1.00 1.00
Quality Control
Here we tabulate the reasons for not using certain digital data sets
The following stations did not have a valid response files:
Last Changed Thu Jul 6 16:26:37 CDT 2017
