实例研究证实，磁组构学方法对于岩浆动力学，特别是岩体构造应力的属性分析非常有效。

This attempt demonstrates that the method of magnetic fabric is effective in the field of magma dynamics, especially for reconstruction of the stress a granite body experienced.

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地震是由于地球内部的岩体受到构造应力作用，导致岩体突然断裂错动的结果。

Earthquake occur because of tectonic stress action from the interior of earth, rock suddenly rupture and slip.

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接触带构造变形特征显示岩体侵位受控于区域左旋剪切应力场作用。

The contact deformation shows that the Fenghuangshan pluton was controlled by a regional sinistral shear stress field.

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