阶梯断层应力场演变特征研究

Guangsheng Chen
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摘要

随着矿山开采向深部发展,地应力也相应增大,地质条件变得越来越复杂。矿山动力灾害主要发生在断层附近。针对单断层的研究较多,但针对复杂地质条件下双断层形成的阶梯状断层的研究较少。基于此,以鹤壁中泰矿业 3110 工作面为工程背景,利用 Flac3D 数值模拟软件建立了单断层模型 a 和不同阶梯断层模型 b、c、d、e、f。研究了单断层和阶梯断层在深部开采影响下的应力场演化特征。结果表明,应力分布在断层上壁形成应力集中区,在下壁形成应力削弱区。在开挖扰动的影响下,断层垂直距离和断层水平距离会影响阶梯断层的应力演化特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on Evolution Characteristics of Stress Field of Stepped Fault
With the development of mining to the deep, the ground stress increases correspondingly, and the geological conditions become more and more complicated. Mine dynamic disasters mainly occur near faults. Numerous studies have been conducted on single faults, but few studies have been done on stepped faults formed by double faults under complex geological conditions. Based on this, with the 3110-working face of Zhong Tai Mining in He bi as the engineering background, Single fault model a and different step fault models b, c, d, e and f were established by Flac3D numerical simulation software. The characteristics of stress field evolution of single fault and step fault under the influence of deep mining are studied. The results show that the stress distribution in the upper wall of the fault forms a stress concentration zone, and in the lower wall forms a stress weakening zone. Under the influence of excavation disturbance, the vertical fault distance and the horizontal distance between faults will affect the stress evolution characteristics of the stepped fault.
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