The paper inverts the focal mechanism solutions of the Yutian M_S7. 3 main shock,foreshocks and M_S≥3. 5 aftershocks by using the CAP method,based on the broadband waveforms recorded by the Xinjiang and Tibet Digital Seismic Networks. The results show that the M_S7. 3 strong earthquake is of strike-slip type with a normal faulting component,and combined with the analysis of focal structure and the aftershock distribution,the nodal plane I with strike 241°,dip 90° and rake- 22° is considered to be the seismogenic fault plane of the main shock. The direction of P-axis for the main shock is 194°,close to the near NS direction of the principal stress P-axis of historical strong earthquakes in this region. The focal mechanism solution of the M_S5. 4 foreshock has a good consistency with that of the main shock. Among the 18 aftershocks,10 are of strike-slip type,6 are of normal faulting type and 2 are of thrust type. 70% of the aftershocks in the sequence have a focal mechanism with P-axis in the near-NS direction. The focal depths of this M_S7. 3 earthquake sequences are distributed in the range of 5km- 28 km,with the majority in the depth range of 15km- 20 km,slightly deeper than the depth of 10 km of the main shock as calculated. The paper inverts the focal mechanism solutions of the Yutian M_S7. 3 main shock, foreshocks and M_S> 3.5 aftershocks by using the CAP method, based on the broadband waveforms recorded by the Xinjiang and Tibet Digital Seismic Networks. The results show that the M_S7. 3 strong earthquake is of strike-slip type with a normal faulting component, and combined with the analysis of focal structure and the aftershock distribution, the nodal plane I with strike 241 °, dip 90 ° and rake- 22 ° is considered to be the seismogenic fault plane of the main shock. The direction of P-axis for the main shock is 194 °, close to the near NS direction of the principal stress P-axis of historical strong earthquakes in this region. The focal mechanism solution of The M_S5. 4 foreshock has a good consistency with that of the main shock. Among the 18 aftershocks, 10 are of strike-slip type, 6 are of normal faulting type and 2 are of thrust type. 70% of the aftershocks in the sequence have a focal mechanism with P- The focal depths of this M_S7. 3 earthquake sequences are distributed in the range of 5km-28 km, with the majority in the depth range of 15km-20 km, slightly deeper than the depth of 10 km of the main shock as calculated.