岩石相互推挤得越厉害，它们就会变得越热；换句话说，不仅是岩石的性质，压力本身也影响摩擦加热。
The harder rocks push against each other, the hotter they become; in other words, pressure itself, not only the rocks' properties, affects frictional heating.
大多数时候，板块之间的摩擦力使两者紧紧挤在一起，并随着时间增加，挤压力逐渐增加。
Most of the time, friction between the plates causes them to stick together, and stress increases over time.
压力于两个板块间积聚而受摩擦力抑制。
Between the two plates, stresses build up that are held in check by friction.
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