The ANSS event ID is ci14408052 and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/ci14408052/executive.
2008/12/06 04:18:42 34.813 -116.419 6.4 5.06 California
USGS/SLU Moment Tensor Solution ENS 2008/12/06 04:18:42:0 34.81 -116.42 6.4 5.1 California Stations used: AZ.LVA2 AZ.PFO AZ.RDM AZ.SOL CI.BAR CI.GLA CI.GSC CI.LDF CI.PASC Filtering commands used: hp c 0.02 n 3 lp c 0.05 n 3 Best Fitting Double Couple Mo = 4.12e+23 dyne-cm Mw = 5.01 Z = 9 km Plane Strike Dip Rake NP1 165 90 -170 NP2 75 80 0 Principal Axes: Axis Value Plunge Azimuth T 4.12e+23 7 300 N 0.00e+00 80 165 P -4.12e+23 7 30 Moment Tensor: (dyne-cm) Component Value Mxx -2.03e+23 Mxy -3.51e+23 Mxz -1.85e+22 Myy 2.03e+23 Myz -6.91e+22 Mzz 0.00e+00 ##------------ ######------------- P ##########------------ --- ###########------------------- ############-------------------- T ############--------------------- # #############--------------------- ##################---------------------- ###################--------------------# ####################----------------###### #####################-----------########## #####################------############### #####################-#################### ###########----------################### ----------------------################## ---------------------################# ---------------------############### --------------------############## -------------------########### ------------------########## ----------------###### ------------## Global CMT Convention Moment Tensor: R T P 0.00e+00 -1.85e+22 6.91e+22 -1.85e+22 -2.03e+23 3.51e+23 6.91e+22 3.51e+23 2.03e+23 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20081206041842/index.html |
STK = 75 DIP = 80 RAKE = 0 MW = 5.01 HS = 9.0
The NDK file is 20081206041842.ndk The waveform inversion is preferred.
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.
USGS/SLU Moment Tensor Solution ENS 2008/12/06 04:18:42:0 34.81 -116.42 6.4 5.1 California Stations used: AZ.LVA2 AZ.PFO AZ.RDM AZ.SOL CI.BAR CI.GLA CI.GSC CI.LDF CI.PASC Filtering commands used: hp c 0.02 n 3 lp c 0.05 n 3 Best Fitting Double Couple Mo = 4.12e+23 dyne-cm Mw = 5.01 Z = 9 km Plane Strike Dip Rake NP1 165 90 -170 NP2 75 80 0 Principal Axes: Axis Value Plunge Azimuth T 4.12e+23 7 300 N 0.00e+00 80 165 P -4.12e+23 7 30 Moment Tensor: (dyne-cm) Component Value Mxx -2.03e+23 Mxy -3.51e+23 Mxz -1.85e+22 Myy 2.03e+23 Myz -6.91e+22 Mzz 0.00e+00 ##------------ ######------------- P ##########------------ --- ###########------------------- ############-------------------- T ############--------------------- # #############--------------------- ##################---------------------- ###################--------------------# ####################----------------###### #####################-----------########## #####################------############### #####################-#################### ###########----------################### ----------------------################## ---------------------################# ---------------------############### --------------------############## -------------------########### ------------------########## ----------------###### ------------## Global CMT Convention Moment Tensor: R T P 0.00e+00 -1.85e+22 6.91e+22 -1.85e+22 -2.03e+23 3.51e+23 6.91e+22 3.51e+23 2.03e+23 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20081206041842/index.html |
** SCSN Moment Tensor Solution Message ** REAL-TIME SOLUTION: OPERATOR REVIEWED Reviewed On: 12/06/2008 4:34:40 Inversion Method: Complete Waveform Number of Stations used: 6 Stations: CI.DSC CI.GMR CI.MCT CI.JVA CI.ADO CI.RRX Real-Time Solution: ------------------- Event ID : 14408052 Magnitude : 5.46 Depth (km) : 6.0 Origin Time : 12/06/2008 04:18:42:550 Latitude : 34.81 Longitude : -116.42 Further Information at: http://pasadena.wr.usgs.gov/recenteqs/Quakes/ci14408052.htm SCSN Moment Tensor Solution: ---------------------------- Moment Magnitude : 5.06 Depth (km) : 5 Variance Reduction(%): 94.07 Quality Factor : A (A : Mw, MT good enough for distribution) (B : Mw only good enough for distribution) (C : Solution needs review before distribution) Best Fitting Double Couple and CLVD Solution: --------------------------------------------------- Moment Tensor: Scale = 10**21 Dyne-cm Component Value Mxx -251 Mxy -375 Mxz -75.6 Myy 326 Myz -73.7 Mzz -74.8 Best Fitting Double Couple Solution: -------------------------------------------------- Moment Tensor: Scale = 10**23 Dyne-cm Component Value Mxx -2.749 Mxy -3.734 Mxz -0.959 Myy 3.052 Myz -0.802 Mzz -0.304 Principle Axes: Axis Value Plunge Azimuth T 4.898 3 296 N 0.000 75 193 P -4.898 15 27 Best Fitting Double-Couple: Mo = 4.90E+23 Dyne-cm Plane Strike Rake Dip NP1 162 -167 82 NP2 70 -8 77 Moment Magnitude = 5.06 ------- ###---------------- #######------------ --- #########------------ P ----- ###########------------ ------- ############---------------------- T ############----------------------- ############------------------------ ################---------------------## #################------------------###### ##################--------------######### ###################---------############# ###################-----################# ###################-##################### ###########--------#################### --------------------################### --------------------################# --------------------############### -------------------############## ------------------########### -----------------######## ---------------#### ------- Lower Hemisphere Equiangle Projection ============= Station Information ============== Name Distance Azimuth VR ZCore ------------------------------------------------- CI.DSC 46.838 37.948 90.911 6.00 CI.GMR 69.614 92.106 94.957 10.00 CI.MCT 73.500 151.611 94.631 10.00 CI.JVA 52.301 199.807 95.550 7.00 CI.ADO 97.276 253.073 93.975 14.00 CI.RRX 53.256 277.985 94.482 8.00 |
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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.
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.
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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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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:
hp c 0.02 n 3 lp c 0.05 n 3The results of this grid search are as follow:
DEPTH STK DIP RAKE MW FIT WVFGRD96 0.5 250 65 -20 4.73 0.4438 WVFGRD96 1.0 75 80 -15 4.74 0.4796 WVFGRD96 2.0 70 70 -25 4.86 0.6214 WVFGRD96 3.0 70 70 -20 4.89 0.6810 WVFGRD96 4.0 75 80 -5 4.90 0.7244 WVFGRD96 5.0 75 80 -5 4.93 0.7586 WVFGRD96 6.0 75 80 -5 4.95 0.7834 WVFGRD96 7.0 75 80 0 4.97 0.8030 WVFGRD96 8.0 75 80 0 5.00 0.8183 WVFGRD96 9.0 75 80 0 5.01 0.8224 WVFGRD96 10.0 75 80 0 5.02 0.8205 WVFGRD96 11.0 75 80 0 5.03 0.8141 WVFGRD96 12.0 75 80 0 5.04 0.8043 WVFGRD96 13.0 75 80 0 5.05 0.7929 WVFGRD96 14.0 75 80 5 5.06 0.7810 WVFGRD96 15.0 75 80 5 5.07 0.7702 WVFGRD96 16.0 75 80 5 5.08 0.7596 WVFGRD96 17.0 75 80 5 5.08 0.7488 WVFGRD96 18.0 75 80 5 5.09 0.7378 WVFGRD96 19.0 75 80 5 5.09 0.7264
The best solution is
WVFGRD96 9.0 75 80 0 5.01 0.8224
The mechanism corresponding to the best fit is
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The best fit as a function of depth is given in the following figure:
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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
hp c 0.02 n 3 lp c 0.05 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. |
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:
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.
The following figure shows the stations used in the grid search for the best focal mechanism to fit the surface-wave spectral amplitudes of the Love and Rayleigh waves.
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The surface-wave determined focal mechanism is shown here.
NODAL PLANES STK= 165.00 DIP= 90.00 RAKE= -165.00 OR STK= 75.00 DIP= 75.00 RAKE= 0.00 DEPTH = 11.0 km Mw = 5.09 Best Fit 0.8665 - P-T axis plot gives solutions with FIT greater than FIT90
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Surface wave analysis was performed using codes from Computer Programs in Seismology, specifically the multiple filter analysis program do_mft and the surface-wave radiation pattern search program srfgrd96.
Digital data were collected, instrument response removed and traces converted
to Z, R an T components. Multiple filter analysis was applied to the Z and T traces to obtain the Rayleigh- and Love-wave spectral amplitudes, respectively.
These were input to the search program which examined all depths between 1 and 25 km
and all possible mechanisms.
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Pressure-tension axis trends. Since the surface-wave spectra search does not distinguish between P and T axes and since there is a 180 ambiguity in strike, all possible P and T axes are plotted. First motion data and waveforms will be used to select the preferred mechanism. The purpose of this plot is to provide an idea of the possible range of solutions. The P and T-axes for all mechanisms with goodness of fit greater than 0.9 FITMAX (above) are plotted here. |
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Focal mechanism sensitivity at the preferred depth. The red color indicates a very good fit to the Love and Rayleigh wave radiation patterns. 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. Because of the symmetry of the spectral amplitude rediation patterns, only strikes from 0-180 degrees are sampled. |
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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