现有的地震资料解释技术都是以连续介质的经典模型为基础的,其理论是把反射界面解释为具有不同弹性模量的两种介质的刚性接触,而反射系数则由声阻抗比来确定。但在实际情况下,找不到能完全对应于记录波场的声阻抗模型。上述情形,正如许多其它事实一样,证明有许多其它机制影响着真实介质普通物理和地震参数的变化。从沉积介质遭受破坏的原因和特点的情况来看,可以提出一些重要的观点。从这个意义上讲,提出缺损介质的破裂模型应被认 Existing seismic data interpretation techniques are based on classical models of continuum media, whose theory is to interpret reflective interfaces as rigid contacts of two media with different moduli of elasticity, and reflection coefficients are determined by acoustic impedance ratios . However, in practical situations, no acoustic impedance model can be found that exactly corresponds to the recorded wavefield. This situation, like many other facts, proves that there are many other mechanisms that influence the variation of ordinary physical and seismic parameters of real media. From the point of view of the causes and characteristics of the destruction of the deposition medium, some important points can be put forward. In this sense, the proposed fracture model of the defect medium should be recognized