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.
实验表明辉长岩岩块在上述正应力下均发生粘滑现象。
Under these normal stresses in experiments on gabbro the stick-slip happened.
以鸡西煤田艳胜井田为例，对断块间褶曲特征、构造应力场及形成机理作初步分析。
For example, Yansheng shaft in Jixi Coal Mine, the character of fault fold, structure stress and forming system are analyzed.
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