引言 实验地震学是地震学的一个重要组成部分,同样也是地震预报学不可缺少的一个分支。自从1962年茂木清夫证实岩石在破裂过程中的微破裂频幅关系与天然地震的频度震级关系同样遵从古登堡-李希特公式后,人们更进一步地将岩石样品和模拟样品的破裂过程与地震实际观测资料进行对比研究,并寄希望于从这类模拟实验研究中得到地震预报的启示。1966年Brace等提出粘滑可能是地震发生的一种物理机制,有关断层粘滑的模拟实验也随之受到更多的重视。伴随实验室研究的深入开展,若干地震震源理论 Introduction Experimental seismology is an important part of seismology and is also an indispensable branch of earthquake prediction. Since 1962, when Mao Mofu confirmed that the relationship between the frequency of micro-rupture of rock during rupture and the magnitude of natural earthquakes follows the Gutenberg-Richter formula, the rupture process of rock samples and simulated samples Compared with the actual observation data of earthquake, we hope that we can get the enlightenment of earthquake prediction from this kind of simulation experiment. In 1966, Brace et al. Proposed that stick-slip may be a physical mechanism for earthquakes and more attention has been paid to the simulation experiments of stick-slip faults. With the further development of laboratory research, a number of earthquake focal theory