因此，当这些应力最终释放的时候，所发生的地震比以往更加具有破坏性，就连在古巴东部就能感受到震动，一系列强烈的余震一直持续到第二天。
When it finally struck, therefore, the earthquake was all the more violent. They could feel the shaking as far away as eastern Cuba.
1967年印度发生的那起震级6.3级、致200人死亡的地震就是印度的柯伊呐(Koyna)大坝(拦截的水产生的应力)造成的。
A magnitude-6.3 quake in India in 1967 that killed 200 people was caused by impoundment behind the country's Koyna Dam.
表明应力应变异常形态的时间特征与地震的孕育和发生有较明显的关系。
The results show that the anomalies' shape character of stress and strain has obvious relation with the development and occurring of earthquakes.
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