AUTOMATIC solution, not reviewed by a seismologist
More details on this rCMT at http://neic.cr.usgs.gov/beta/rcmt/events/100117060437.2010rpai
usr/passwd : rcmt/rcmt
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General region :  2010rpai OFF EAST COAST OF HONSHU,                         
surface waves  (3.0,3.5,7,7.5 mHz)
Stations used :  AAK ARU CTAO LVZ PMG TLY ULN YAK                                                                   
Origin time: 2010   17   6   4  37
Original location (lat,lon,depth) :      38.0000    143.600  12   
Moment tensor (x1.e26 dyncm) :
Mrr :     -0.016871 Mtt :     -0.018258
Mff :      0.035129 Mrt :     -0.028836
Mrf :      0.021740 Mtf :      0.014470
T-axis:  moment=     0.043   plunge=    17.711  azimuth=   274.852    
N-axis:  moment=     0.010   plunge=    41.248  azimuth=   168.590    
P-axis:  moment=    -0.054   plunge=    43.438  azimuth=    22.454    
best double couple: Mo=    0.049(x1.e26 dyncm)  Mw=5.7  tau=  2.0     
nodal planes (strike/dip/slip):   48.21/ 45.47/-22.35     154.29/ 74.27/-133.23 
Centroid location :   38.143   143.432    33.781
Centroid time :     19.282
Variance reduction (%) :  21.2
 
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        *------- o          P         o *   
       *---------oo                   o  *  
      **--------- o                   o  ** 
      *-----------oo                 oo  -* 
     **--T---------oo                o  --**
     **-------------o   +           oo ---**
     **-------------oo             oo-----**
      *--------------oo-         ooo------* 
      **--------------oo----  --oo-------** 
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               ****-----------****          
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          0-   30-  60-  90-  120- 150- 180- 210- 240- 270- 300- 330-           
z-comp:     1    0    0    0    0    0    2    2    1    0    0    0            
r-comp:     0    0    0    0    0    0    0    1    0    0    0    0            
t-comp:     1    0    0    0    0    0    1    3    0    0    0    0            
Total number of traces used =  12  
number of runs = 11
starttime = Sat Jan 16 23:20:51 MST 2010
Solution produced by inversion of channels with var red > 2%