AUTOMATIC solution, not reviewed by a seismologist
More details on this rCMT at http://neic.cr.usgs.gov/beta/rcmt/events/090716175935.2009jdbf
usr/passwd : rcmt/rcmt
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General region :  2009jdbf VANUATU                                           
surface waves  (3.0,3.5,7,7.5 mHz)
Stations used :  CASY CTAO INCN KIP MAJO PMG RPN TAU                                                                
Origin time: 2009  197  17  59  35
Original location (lat,lon,depth) :     -17.6000    167.700  10   
Moment tensor (x1.e26 dyncm) :
Mrr :      0.052856 Mtt :     -0.006689
Mff :     -0.046166 Mrt :      0.020654
Mrf :     -0.016905 Mtf :      0.002289
T-axis:  moment=     0.062   plunge=    71.553  azimuth=    26.842    
N-axis:  moment=    -0.012   plunge=    14.718  azimuth=   168.793    
P-axis:  moment=    -0.050   plunge=    10.873  azimuth=   261.685    
best double couple: Mo=    0.056(x1.e26 dyncm)  Mw=5.8  tau=  2.1     
nodal planes (strike/dip/slip):    9.61/ 36.47/115.30     159.16/ 57.49/ 72.47  
Centroid location :  -17.316   167.951    33.752
Centroid time :      3.279
Variance reduction (%) :  19.8
 
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        *     -o------------------oo--  *   
       *      -o-------------------o---  *  
      **      -o-------------------oo--  ** 
      *        oo---------T---------o--   * 
     **        -o-------------------o--   **
     **         oo------+-----------o-    **
     ** P       -o-----------------oo-    **
      *          oo----------------o-     * 
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       *           oo-------------o-     *  
        *           oo----------oo      *   
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          0-   30-  60-  90-  120- 150- 180- 210- 240- 270- 300- 330-           
z-comp:     0    0    1    0    0    0    1    1    1    1    1    1            
r-comp:     0    0    0    0    0    0    1    0    0    1    1    0            
t-comp:     0    0    0    0    1    0    1    0    0    1    1    0            
Total number of traces used =  14  
number of runs = 14
starttime = Thu Jul 16 12:20:38 MDT 2009
Solution produced by inversion of channels with var red > 2%