Mechanism of the June 4, 2000 southern Sumatra, Indonesia, earthquake (MS=8.0) are estimated from teleseismic body waves recorded by long period seismograph stations of the global seismic network. This solution is more reasonable than those reported by USGS, Harvard CMT and ERI of University of Tokyo. The best double-couple component of this earthquake is 1.51021 Nm, the compensated linear vector dipole component is 1.21020 Nm, and the explosion component is 5.91019 Nm. The focal mechanism is mainly left-lateral strike-slip, with a small thrust component. Nodal plane I: The strike is 199? the dip, 82? and the rake, 5? Nodal plane II: The strike is 109? the dip, 85, and the rake, 172. P axis: The azimuth is 154 and the plunge, 2; T axis: The azimuth is 64 and the plunge, 10; B axis: The azimuth is 256 and the plunge, 80. The P-waveforms recorded at different stations show prominent directivity. The directivity shows that the Nodal plane I is the fault plane, and that the earthquake ruptured unilaterally from the northeast to the southwest, nearly perpendicular to the strike of the Java trench.
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