The strain state of the emplaced magma is shown by ellipsoid parameters, and distribution of stress field of the magma reflects the ways of emplacement and tectonic environment.

• 从磁化率椭球参数可以看出岩浆侵位的应变状态；岩浆应力场分布体现了岩浆侵位元方式及其所处构造坏境。