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.
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.
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.
同时，对用弹性波法确定岩体地应力及水平构造应力进行了探讨。
At a time the acoustic measurement method of rock mass stresses and the horizontal tectonic stress are discussed.
同时，对用弹性波法确定岩体地应力及水平构造应力进行了探讨。
At a time, the acoustic measurement method of rock mass stresses and the horizontal tectonic stress are discussed.
从岩石、岩体构造、原岩应力、水文地质条件、工程设计和施工因素以及围岩应力等六个方面论述和探讨了现场岩爆发生的条件。
The Conditions of in situ rock-burst were probed into from rocks, rock mass structure, in-situ stress, hydrological conditions, engineering design and construction factors.
结果表明：计算值能够较好地拟合实测值，证明自重应力水平构造应力是形成地应力主要因素。根据回归分析结果，获得了整个工程区域岩体的地应力分布。
The regression output shows that the calculated stress match the measured data, also the gravity and horizontal tectonic stress are the main factors of the stress field in the project area.
深部岩体具有典型的不均匀、不连续的自应力块系等级构造结构。
Deep rock mass has a typical inhomogeneous and discontinuous self-stressed block-hierarchical structure.
深部岩体具有典型的不均匀、不连续的自应力块系等级构造结构。
Deep rock mass has a typical inhomogeneous and discontinuous self-stressed block-hierarchical structure.
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