结果表明，磁化率椭球与应变椭球之间，显示了密切的相关性。

The results indicate that an obvious correlation appears between the susceptibility ellipsoid and the strain ellipsoids.

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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方式及其所处构造环境。

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.

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主应变的大小和方向可以表示为一个椭球体。

The magnitudes and directions of the main strain are expressed as an ellipsoid.

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