It is shown that regional initial rock stress state is controlled by larger faults and that heterogeneity and aeolotropism of initial rock stress field are caused by superposition of action of faults.
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研究结果表明:区域原岩应力状态宏观上主要受几何尺寸大的断层的支配,局部范围内受复合断层的叠加扰动影响,造成了原岩应力状态的各向异性及非均匀分布特征。
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