【摘 要】
：
依据已有的一些力学分析结果、模型模拟结果和地质体中构造变形破坏的特征，指出层状岩体垒积序列差异性是控制地质体在法向上构造变形破坏的内因．并建立了定量描述它的ＳＣＷＲ／Ｓ分形模
【机 构】
：
东北大学资源与土木工程学院,长春科技大学
论文部分内容阅读
依据已有的一些力学分析结果、模型模拟结果和地质体中构造变形破坏的特征，指出层状岩体垒积序列差异性是控制地质体在法向上构造变形破坏的内因．并建立了定量描述它的ＳＣＷＲ／Ｓ分形模型，使得不同地质体的差异性具有定量可比性；同时初步推测了它与构造变形间的表观关系．
Based on some existing mechanical analysis results, model simulation results and the characteristics of structural deformation and deformation in the geological body, it is pointed out that the difference of the stacking sequence of layered rock mass is the internal cause for controlling the deformation and failure of the geological body in the normal direction. And established a SCWR / S fractal model that quantitatively describes it, which makes the difference of different geological bodies quantitatively comparable. At the same time, it preliminarily estimates the apparent relationship between it and tectonic deformation.
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