Location

2006/05/10 02:42:56 52.71 -169.24 56

Moment Tensor Comparison

The following compares this source inversion to the USGS Rapid Moment Tensor Solution and to the Harvard CMT solutions, if they are available.

Note that the SLU solution agrees better with historical mechanisms there than either the Harvard or USGS solutions ( Other moment tensors )
SLU
USGS
HARVARD CMT
Mw=6.2  

2006/05/10 02:42:56    EVID:  
LAT: 52.71N, LON: 169.24W, DEPTH:  25
Mw: 6.2, mb: 0.0, Ms: 0.0
Mo=  0.260E+26 (dyne-cm)
  
No. of Stations:  67, GAP:  59
Error (clvd/dc)*100=  48.48
Bandpass:  12 -  60 sec
Nodal plane parameters
      strike     dip    rake
NP1:      80      73      84
NP2:     279      18     108
       
             ---------------             
          ---------------------          
       ----#################------       
     ---########################----     
    --############################---    
   -#############   ################--   
  -############## T #################--  
 -###############   ##################-- 
 ######################################- 
 #####################################-# 
 ##################################----- 
 #############################---------- 
 -######################---------------- 
 --------------------------------------- 
  -------------------------------------  
   -----------------------------------   
    ---------------------------------    
     ---------------   -------------     
       ------------- P -----------       
          ----------   --------          
             ---------------             
                                         

Stat Dist Az Misfit   Stat Dist Az Misfit
116A  45  92  0.53    ACSO  57  65  0.27
AFI   66 182  0.68    AQU   85 358  0.23
ARU   64 332  0.16    BBSR  72  58  0.31
BNLO  36  96  0.89    CBKS  48  77  0.42
CEL   89 355  0.15    CHTO  76 282  0.21
CWC   39  93  0.92    D04A  29  81  0.76
DAV   69 254  0.52    DPC   77 356  0.16
EIDS  85 215  0.86    EKS2  70 315  0.21
ESK   71   8  0.22    FITZ  90 239  0.59
GRFO  77 359  0.14    GUMO  53 240  0.31
GVD   92 349  0.27    HNR   67 213  0.66
ISCO  44  80  0.48    KIP   32 160  0.66
KIV   79 337  0.20    L02A  32  90  0.82
LGU   39  97  0.82    M05C  34  89  0.70
MALT  86 338  0.22    MAUI  33 157  0.62
MNTX  49  88  0.43    N02C  33  92  0.89
O05C  35  91  0.68    OBIP  83  69  1.00
OUZ   88 193  0.72    PAB   87  11  0.18
PMG   72 225  0.46    POHA  34 156  1.08
PPCW  55  67  0.99    RAR   74 170  0.99
RUE   75 358  0.18    S05C  37  94  0.85
SANT  90 348  0.31    SDV   88  77  0.31
SLM   54  71  0.32    SNZO  94 192  0.85
SSB   82   4  0.26    STKA  94 220  0.57
STU   78   1  0.20    TKM2  69 314  0.13
TRO   41  95  0.73    TUC   46  92  0.48
TUE   81   0  0.20    TUQ   40  93  0.79
ULN   50 300  0.27    URZ   91 190  0.95
USIN  56  70  0.24    VSU   68 351  0.16
VTS   84 350  0.17    WRAB  87 231  0.52
X15A  43  91  0.58    Y12C  42  93  0.63
Y22C  47  87  0.44    YNG   94 214  0.64
YSS   31 278  0.27    YULB  59 268  0.37
ZKR   91 347  0.27
 Misfit > 1 heavily downweighted
	
Mw=6.2 FOX ISLANDS, ALEUTIAN ISLANDS

2006/05/10 02:42:56.30    EVID: MNAG
LAT: 52.71N, LON: 169.24W, DEPTH:  30
Mw: 6.2, mb: 6.3, Ms: 6.3
Mo=  0.203E+26 (dyne-cm)

No. of Stations:  13, GAP: 175
Error (clvd/dc)*100=  14.43

Nodal plane parameters
      strike     dip    rake
NP1:      59      53      88
NP2:     243      37      93

                ----------
           --------------------
        --------------------------
      -----------------#####--------
     ------------##################--
    ---------#########################
   --------###########################-
  -------#############################--
  -----##############################---
 -----##############################-----
 ----##############################------
 ---##############################-------
 ---############################---------
  -###########################----------
  -#########################------------
   ######################--------------
    #################-----------------
     --------------------------------
      ------------------------------
        --------------------------
           --------------------
                ----------

Stat Dist Az Misfit   Stat Dist Az Misfit
ANMO  47  86  0.39    FCC   40  50  0.41
FFC   38  59  0.45    HKT   56  82  0.53
HLID  36  81  0.95    ISCO  44  80  0.46
KBS   48 359  0.38    MAJO  39 267  0.93
RSSD  42  74  0.27    TUC   46  92  0.56
WDC   33  92  0.88    YAK   33 310  0.64
YSS   31 278  0.34

Median of misfit:  0.46
  Average misfit:  0.55

        
May 10, 2006, FOX ISLANDS, ALEUTIAN ISLANDS, MW=6.4

Natasha Maternovskaya

CENTROID, MOMENT TENSOR SOLUTION
HARVARD EVENT-FILE NAME C051006A
DATA USED: GSN
L.P. BODY WAVES: 87S,230C, T= 40
MANTLE WAVES:    79S,170C, T=125
CENTROID LOCATION:
ORIGIN TIME       02:42:56.5 0.1
LAT 52.24N 0.01;LON 169.25W 0.01
DEP  31.7 0.5;HALF-DURATION  3.9
MOMENT TENSOR; SCALE 10**25 D-CM
  MRR= 3.66 0.03; MTT=-3.20 0.03
  MPP=-0.46 0.03; MRT= 2.99 0.08
  MRP= 1.51 0.07; MTP=-1.49 0.02
 PRINCIPAL AXES:
 1.(T) VAL=  4.94;PLG=69;AZM=331
 2.(N)       0.19;     2;     65
 3.(P)      -5.13;    21;    156
BEST DOUBLE COUPLE:M0=5.0*10**25
 NP1:STRIKE=249;DIP=24;SLIP=  94
 NP2:STRIKE= 64;DIP=66;SLIP=  88

            -----------
        -------------------
      -------############----
    ------###################--
   ----########################-
  ----########   ###############-
  --########## T ##############--
 --###########   ############-----
 --#########################------
 -#######################---------
 -#####################-----------
  #################--------------
  #############------------------
   -----------------------------
    -----------------   -------
      --------------- P -----
        -------------   ---
            -----------

        

Deviatoric Moment Tensor Solution

The following broadband stations were used for the source inversion: 116A ACSO AFI AQU ARU BBSR BNLO CBKS CEL CHTO CWC D04A DAV DPC EIDS EKS2 ESK FITZ GRFO GUMO GVD HNR ISCO KIP KIV L02A LGU M05C MALT MAUI MNTX N02C O05C OBIP OUZ PAB PMG POHA PPCWF RAR RUE S05C SANT SDV SLM SNZO SSB STKA STU TKM2 TRO TUC TUE TUQ ULN URZ USIN VSU VTS WRAB X15A Y12C Y22C YNG YSS YULB ZKR



Location of the earthquake (yellow star) and great circle path from the epicenter to each station (red) [created using GMT (Wessel, P., and W. H. F. Smith, New version of Generic Mapping Tools released, EOS Trans. AGU, 76 329, 1995.)]

All observed and Greens function waveforms are corrected to instrument response to ground velocity in meters/sec for the passband of 0.01 - 5 Hz. Next tre traces were bandpass filtered by the application of the following high- and low-pass stages:

hp c 0.0167 2
lp c 0.0833 2
The traces were next integrated to ground displacment in meters. Finally waveforms were cut from 30 seconds before to 140 seconds after the P arrival so that the direct P wave, pP and perhaps the sP are included.

The source inversion is a multipass operation since a lower frequency filter band is used for larger earthquakes and since a search is made over depth. Up to three passed of the outer loop are made, after which the moment magnitude is determined and filter settings readjusted. The inner loop over depth samples all depths from 0 to 800 km with 5 km increments in depth to 50 km, followed by 10 km depth sampling for the remaining range.

The following filter ranges are used according to the moment magnitude Mw:

   FILTER_BAND   FH(s)  FL(s)
       1           60     12      Mw < 6.4
       2          100     20      6.4 < Mw <= 6.9
       3          120     40      Mw > 6.9

For this data set the favored solution is

WVFMTD96   25.0   80.   73.   84.   6.24     0.006 0.132E-04     0.506     0.085 0.687E-06  48.5

The following figures show the sensitivity of the goodness of fit parameter so source depth, the waveform comparison as a function of epicentral distance in degrees and the source to station azimuth

Depth Sensitivity

Goodness of fit as a function of source depth. The measure is 1 - SUM (o -p)2 / SUM o2. A value of 1.0 is the best fit. The best double couple mechanism for the solution depth is plotted above goodness of fit value to indicate how the mefhanism may change with depth.

Fit with Distance

Comparison of the observed traces (red) and solution predicted traces (blue) as a function of epicentral distance in degrees (D). For ease of comparison, the time axis is T - p D, where p is 5.0 seconds/degree and T is the actual travel time. The traces are annotated with the station name at the top.

Fit with Azimuth

Comparison of the observed traces (red) and solution predicted traces (blue) as a function of source to station azimuth in degrees (D). The purpose of this display is to highlight the azimuthal dependence on the first motion. The traces are annotated with the station name at the top.

Inversion Details

Output of wvfmtd96 for the best depth..

Last Changed Fri May 12 18:08:35 UTC 2006