This paper deals with some results of experimental study on semi-brittle behavior of rocks at the conditions relevant to the middle-lower crust.
本文着重介绍了在中下地壳温度、压力条件下进行的几种岩石半脆性蠕变的实验研究结果。
With the decreasing of heterogeneity , the main failure process presents brittle behavior , and vice versa , with the increasing of heterogeneity , failure process presents ductile behavior.
随著非均匀程度的降低，主破裂呈现脆断模式，而随著非均匀程度的增加而呈现韧性破坏特征。
The research method and conclusions can be used to analyze the dynamic behavior of the other brittle materials.
该方法与结论对其他类型的脆性材料的动态性能研究具有一定的参考价值。
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