Therefore it is considered that interaction between low velocity layer and fault could be one of the main physical property and structural environment in seismogenesis.
故认为低速层和断层的作用可能是地震孕育的主要物性和结构环境因素之一。
2
Moreover, by combining with the influence field, seismotectonic environment and focal mechanism solution, some problems related to seismogenesis are also discussed in this paper.