These interactions may also serve as important ways for lithosphere recycling and mass exchange between the shallow and 这种相互作用被认为是稳定克拉通岩石圈遭受改造甚至破坏的深部机制，同时还是地球深、浅部物质交换的重要方式，因而显著影响着地球深部的对流和地表的构造过程。