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Study On The Law Of Ground Strata Subsidence And Movement Induced By Caving Mining Of Slowly Inclined Large And Thick Ore Body

机译:塌陷大型厚矿体塌陷矿井地下地层沉降和运动的研究

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Taking the Western District of Chengchao Iron Mine as engineering background, based on the GPS monitoring data of nearly 8 years and the record of the ground surface movement, the law of ground strata subsidence and movement is studied. The studies have shown that the surface movement caused by underground mining has the characteristics of time delay and displacement angle development has the law of jumping. The strata movement caused by mining is divided into the stage of overlying strata collapse and the collapse stage of surrounding rock to goaf. In the first stage, the vertical stress plays a leading role and rock failure is shown as a regular barrel collapse. In the second stage, horizontal tectonic stress plays a leading role and the collapse mechanism of rock strata can be explained by the cantilever beam theory. According to the mechanism of strata movement analysis, strata movement of Chengchao Iron is divided into six regions, which respectively included vertical subsidence area, toppling sliding zone, dumping area, deformation zone, cumulative deformation area and undisturbed zone. The results of this paper can provide a theoretical basis for the surface movement prediction of caving mining in similar metal mine.
机译:以城区区区为工程背景,基于GPS监测数据近8年,地面运动的记录,研究了地层沉降和运动的规律。这些研究表明,由地下挖掘引起的表面运动具有时间延迟和位移角度发展的特点。采矿引起的地层运动被分为覆盖地层崩溃的阶段和周围岩石的崩溃阶段。在第一阶段,垂直压力起到主导作用,并且岩石破坏被显示为常规桶崩溃。在第二阶段,水平构造应力起到主要作用,并且可以通过悬臂梁理论解释岩石地层的折叠机构。根据地层运动分析的机制,成越铁的地层运动被分成六个区域,分别包括垂直沉降区域,倒装滑动区域,倾倒区域,变形区,累积变形区域和未受干扰区域。本文的结果可以为类似金属矿井的煤矿开采的表面运动预测提供理论依据。

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