本文以应力释放模型为基础，为研究大震增(减)震问题对模型提出改进。
Based on the Stress Release model, this article has improved the model in order to study the strong earthquake increase (decrease) earthquake problem.
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。
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.
通过对应力—强度干涉模型的分析，针对安全部件专用电磁铁的特性，提出了安全部件专用电磁铁的释放可靠性理论。
In the condition of assuming that stress and intensity obey normal distribution, the basic method of reliability design, stress-intensity interference model is discussed.
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