The underground tear started 100 kilometers off the coast of Sumatra, on the western edge of the Burma plate.
地壳由印尼苏门达腊外海100公里处开始破裂，那里是缅甸板块的西侧边缘。
The theoretical stress releasing period of crust and mantle in India and Burma plate is calculated by viscoelastic model. It is about 56a and close to the strong earthquake activity period.
利用粘滞模型计算了印缅板块地区壳幔的理论应力释放周期为56年，与该地区的强震活动周期基本吻合。
It was caused by a megathrust event as the India plate moved beneath the Burma microplate.
它是由印度板块在缅甸微板块下移动时发生的大型逆冲事件引起的。
It was caused by a megathrust event as the India plate moved beneath the Burma microplate.
它是由印度板块在缅甸微板块下移动时发生的大型逆冲事件引起的。
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