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为了研究断层的深部构造和深部断层物质的力学性质,在国外曾有人对一些大断裂带进行过地球物理勘探,得到横跨断裂带的速度剖面和密度剖面。在物探资料的反演过程中,由于构造和物性二者均是未知的因素,取得断层物质高压状态参量的实验数据是有意义的。人
In order to study the deep structure of faults and the mechanical properties of deep fault, some people in other countries conducted geophysical prospecting for some large fault zones, and obtained the velocity profile and density profile across the fault zone. During the inversion of geophysical data, it is significant to obtain the experimental data of the high-pressure state parameters of the fault because the structure and physical properties are unknown. people