中源地震脱水脆变机制的岩石学研究进展

夏阳, 张立飞^*

The Advance of Petrologic Mechanism of Dehydration Embrittlement in Intermediate-depth Earthquakes

Xia Yang, Zhang Lifei

图5 断层微结构：实验室模拟1～6 GPa条件下蛇纹石的脱水脆变 [ 5 ]
Fig. 5 Fault microstructure. In all conditions tested 1～6 GPa in the lab, the embrittlement of antigorite serpentinite during dehydration [ 5 ]