Location

2005/01/28 22:37:07 34.71 111.00 3 4.0 ARIZONA

Arrival Times (from USGS)

Arrival time list

Felt Map

USGS Felt map for this earthquake

USGS Felt reports page for Intermountain Western US

Focal Mechanism

The focal mechanism was determined using broadband seismic waveforms. The location of the event and the station distribution are given in Figure 1.
Figure 1. Location of broadband stations used to obtain focal mechanism

The preferred solution from an analysis of the surface-wave spectral amplitude radiation pattern, waveform inversion and first motion observations is

      STK = 135
      DIP = 75
     RAKE = -15
       MW = 3.76
       HS = 4

Waveform Inversion

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:

hp c 0.02 3
lp c 0.06 3
The results of this grid search from 0.5 to 19 km depth are as follow:

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96    0.5   140    85    10   3.61 0.7012
WVFGRD96    1.0   140    80     5   3.63 0.7269
WVFGRD96    2.0   140    85     5   3.68 0.7750
WVFGRD96    3.0   315    80   -20   3.73 0.7997
WVFGRD96    4.0   135    75   -15   3.76 0.8081
WVFGRD96    5.0   130    65   -20   3.82 0.8053
WVFGRD96    6.0   130    65   -15   3.85 0.7866
WVFGRD96    7.0   315    65     0   3.85 0.7655
WVFGRD96    8.0   315    55     0   3.88 0.7534
WVFGRD96    9.0   320    75    30   3.88 0.7463
WVFGRD96   10.0   320    70    25   3.89 0.7420
WVFGRD96   11.0   325    65    30   3.87 0.7428
WVFGRD96   12.0   325    65    30   3.88 0.7432
WVFGRD96   13.0   325    65    30   3.88 0.7419
WVFGRD96   14.0   325    60    25   3.88 0.7408
WVFGRD96   15.0   325    65    25   3.88 0.7388
WVFGRD96   16.0   325    65    25   3.88 0.7366
WVFGRD96   17.0   325    65    25   3.88 0.7327
WVFGRD96   18.0   325    65    20   3.88 0.7286
WVFGRD96   19.0   325    65    20   3.89 0.7251

The best solution is

WVFGRD96    4.0   135    75   -15   3.76 0.8081

The mechanism correspond to the best fit is
Figure 1. Wavefrom inversion focal mechanism

The best fit as a function of depth is given in the following figure:

Figure 2. Depth sensitivity for waveform mechanism

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 componnet is plotted to the same scale and peak amplitudes are indicated by the numbers to the left of each trace. The number in black at the rightr of each predicted traces 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 bandpass filter used in the processing and for the display was

hp c 0.02 3
lp c 0.06 3
Figure 3. Waveform comparison for depth of 8 km

Surface-Wave Focal Mechanism


  NODAL PLANES 

  
  STK=      79.99
  DIP=      49.99
 RAKE=    -115.00
  
             OR
  
  STK=     295.95
  DIP=      46.03
 RAKE=     -63.28
 
 
DEPTH = 3.0 km
 
Mw = 3.83
Best Fit 0.8874 - P-T axis plot gives solutions with FIT greater than FIT90

Surface-Wave Focal Mechanism

First motion data

The P-wave first motion data for focal mechanism studies are as follow:

Sta Az(deg)    Dist(km)   First motion
TUC       176  267 eP_+
GLA       244  399 eP_X
MVU       346  434 eP_X

Surface-wave analysis

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.

The velocity model used for the search is a modified Utah model .

Data preparation

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.
Best mechanism fit as a function of depth. The preferred depth is given above. Lower hemisphere projection

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.


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. A nearly vertical strike-slip fault striking at 75 or 165 degrees is preferred. Because of the symmetry of the spectral amplitude rediation patterns, only strikes from 0-180 degrees are sampled.

Love-wave radiation patterns

Rayleigh-wave radiation patterns

Broadband station distributiuon

Sta Az(deg)    Dist(km)   
TUC	  176	  267
PDM	  262	  292
GLA	  244	  399
DAN	  270	  402
MVU	  346	  434
SHO	  287	  497
SDCO	   54	  598
MNTX	  121	  621
GRA	  296	  628
TPH	  306	  671
ISCO	   39	  739
MNV	  305	  761
HWUT	  356	  767
BMN	  321	  839
AHID	  360	  894
BW06	    8	  903
LTX	  129	  913
CMB	  296	  919
HLID	  344	 1026
WVOR	  324	 1084
LKWY	    2	 1095
WMOK	   86	 1118
JCT	  111	 1150
WDC	  306	 1207
BOZ	  358	 1216
MSO	  350	 1368
KSU1	   65	 1370
LAO	   15	 1390
COR	  320	 1519
NEW	  343	 1589
OCWA	  327	 1816
FVM	   73	 1878
SLM	   71	 1902
BLO	   70	 2229
WCI	   73	 2242
ERPA	   64	 2813
SSPA	   67	 2976
SDMD	   70	 3064
HRV	   64	 3510

Waveform comparison for this mechanism

Since the analysis of the surface-wave radiation patterns uses only spectral amplitudes and because the surfave-wave radiation patterns have a 180 degree symmetry, each surface-wave solution consists of four possible focal mechanisms corresponding to the interchange of the P- and T-axes and a roation of the mechanism by 180 degrees. To select one mechanism, P-wave first motion can be used. This was not possible in this case because all the P-wave first motions were emergent ( a feature of the P-wave wave takeoff angle, the station location and the mechanism). The other way to select among the mechanisms is to compute forward synthetics and compare the observed and predicted waveforms.

The velocity model used for the waveform fit is a modified Utah model .

The fits to the waveforms with the given mechanism are show below:

This figure shows the fit to the three components of motion (Z - vertical, R-radial and T - transverse). For each station and component, the observed traces is shown in red and the model predicted trace in blue. The traces represent filtered ground velocity in units of meters/sec (the peak value is printed adjacent to each trace; each pair of traces to plotted to the same scale to emphasize the difference in levels). Both synthetic and observed traces have been filtered using the SAC commands:

hp c 0.02 3
lp c 0.06 3
br c 0.1 0.2 n 8 p 2

Discussion

The Future

Should the national backbone of the USGS Advanced National Seismic System (ANSS) be implemented with an interstation separation of 300 km, it is very likely that an earthquake such as this would have been recorded at distances on the order of 100-200 km. This means that the closest station would have information on source depth and mechanism that was lacking here.

Acknowledgements

Dr. Harley Benz, USGS, provided the USGS USNSN digital data.

Appendix A

The figures below show the observed spectral amplitudes (units of cm-sec) at each station and the theoretical predictions as a function of period for the mechanism given above. The modified Utah model earth model was used to define the Green's functions. For each station, the Love and Rayleigh wave spectrail amplitudes are plotted with the same scaling so that one can get a sense fo the effects of the effects of the focal mechanism and depth on the excitation of each.

Quality Control

Here we tabulate the reasons for not using certain digital data sets

Last Changed Wed Oct 19 12:41:48 CDT 2005