沟道应力的模拟方法则采用掩膜版边缘错位模型(mask - edge dislocation model)，应力测量方面采用拉曼光谱法。
Channel stress is simulated by using mask-edge dislocation model and actual stress is also measured by Raman spectroscopy.
某些远离板块边缘的“错位”火山是由另一种独立机制造成的，这种机制能够使地球内部深处的温度降低。
Certain "misplaced" volcanoes far from plate edges result from a second, independent mechanism that cools the deep interior of Earth.
某些远离板块边缘的“错位”火山是由另一种独立机制造成的，这种机制能够使地球内部深处的温度降低。
Certain "misplaced" volcanoes far from plate edges result from a second, independent mechanism that cools the deep interior of Earth.
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