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Mining-induced ground deformation in tectonic stress metal mines: A case study

机译:构造应力金属矿山采矿引起的地面变形:案例研究

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In situ monitoring data of ground deformation in the western area of Chenchao Iron Mine were collected over eight years. Results were analysed to conduct a preliminary investigation into the ground movement induced by underground mining: (1) in the northeastern area, the ratios of horizontal to vertical displacement increase gradually, and the horizontal displacement may be as much as an order of magnitude larger than the vertical displacement at a large distance, which induces regional horizontal movement Curves of the ratio of horizontal to vertical displacement with respect to time can be categorised as: fluctuation-, fallback-, convergence-, and increase-types; (2) in the mine road, stack-site, and southern area around the high-voltage tower, ground deformation can be divided into two stages: stable deformation and rapid deformation. While in the southeastern area of the transport tunnel, service shaft, and road tunnel, it can be divided into three stages: stable deformation, rapid deformation, and subsequent stable deformation. Three categories are found in the time-displacement curves: folding-, S-, and linear-types. (3) The ground deformation of the footwall underwent a significant change in January 2010, because the large horizontal tectonic-stress in the mine was released at that time. Surrounding rock masses were subjected to toppling deformation along the major structural plane in the northeastern area, while tensile deformation occurred perpendicular to the major structural plane in the northern area. (C) 2016 Elsevier B.V. All rights reserved.
机译:陈潮铁矿西部地区地面变形监测数据历时八年。分析结果对地下采矿引起的地面运动进行了初步调查:(1)在东北地区,水平位移与垂直位移之比逐渐增大,水平位移可能比垂直位移大一个数量级。远距离的垂直位移会引起区域水平运动。水平位移与垂直位移之比相对于时间的曲线可分为:波动型,后退型,会聚型和增加型。 (2)在矿山道路,堆场和高压塔周围的南部地区,地面变形可分为两个阶段:稳定变形和快速变形。在运输隧道,服务井和公路隧道的东南区域,它可以分为三个阶段:稳定变形,快速变形和随后的稳定变形。在时间-位移曲线中可以找到三种类型:折叠型,S型和线性型。 (3)2010年1月,由于当时释放了巨大的水平构造应力,下盘的地面变形发生了重大变化。在东北地区,围岩沿主结构面发生倾覆变形,而在北部地区,垂直于主结构面发生拉伸变形。 (C)2016 Elsevier B.V.保留所有权利。

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