Thus the deformation of enclaves are modeled with physical process of the interaction between enclaves and their host magmas. As the result, the real ascent rate of the host magma with the field data about the size deformation degree can be determined.

• 因此，可用包体与岩浆相互作用的物理过程来模拟包体的变形特点，而反过来据实测的包体变形程度数据又可推算岩浆真实的上升速度