序言 刚性的岩石圈板块是瞬时板块构造理论的基本前提之一。板块边界构造活动和变形的型式和关系过去已有研究;但是相互作用力的详细性质却远不了解。 应力的最好标志之一是地震的发生,如果承认板块刚性这个基本前题,那末同一板块边界之间的相互动力作用也可以传播到另 Preface The rigid lithospheric plate is one of the basic preconditions for the theory of tectonic plate. The types and relationships of tectonic activity and deformation in the plate boundaries have been studied in the past; however, the detailed nature of the interaction forces is far from understood. One of the best signs of stress is the occurrence of earthquakes. If one acknowledges the basic proposition of plate rigidity, the interaction between the same plate boundaries can also be propagated to another