峻德井田断裂构造的分形特征及对冲击地压的控制作用
Fractal characteristics of fault structure and its control effect on rock burst in Junde minefield
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摘要: 为研究鹤岗煤田南部矿区峻德井田断裂构造对冲击地压的控制作用,基于地质动力区划法、层次分析法和脆弱性指数法。以峻德煤矿17煤层为研究对象,运用分形理论,对Ⅰ~Ⅴ级断块进行了分形计算和特征分析。针对峻德煤矿17煤层冲击地压严重性,划分17煤层构造应力分区,分析断裂构造分形维数与构造应力状态、冲击地压之间的相关关系。结果表明:从整体分维角度看,峻德井田的Ⅴ级断块具有统计自相似性和空间几何分形特征;断裂的整体分形维数为1.2714,其中NE向断裂分形维数为1.0964,NW向断裂分形维数为1.1236,表明了NW向断裂对峻德煤矿的冲击地压起控制作用,而NE向断裂对冲击地压具有重要的影响。运用层次分析法确定各影响因素的权重,结合GIS软件对其进行归一化处理,并进行叠加,将研究区划分为四个区域,以往的冲击地压事故多发生在危险区,与实际情况相符。该研究方法为冲击地压灾害防治提供科学依据。Abstract: In order to study the control effect of fault structure on rock burst in Junde mine field, southern mining area of Hegang coalfield, the control effect of fault structure on rock burst was studied., based on geodynamic zoning method, analytic hierarchy process and vulnerability index method.Taking the 17 coal seam of Junde Coal Mine as the research object, the fractal calculation and fea-ture analysis of I ~ V fault blocks are carried out by using fractal theory.In view of the seriousness of rock burst in 17 coal seam of Junde Coal Mine, the tectonic stress zoning of 17 coal seam is divided, and the correlation between fractal dimension of fault structure, tectonic stress state and rock burst is analyzed.The results show that from the perspective of overall fractal dimension, the V-level fault block in Junde mine field has statistical self-similarity and spatial geometric fractal characteristics.The overall fractal dimension of the fault is 1.2714, of which the fractal dimension of the NE-trending fault is 1.0964, and the fractal dimen-sion of the NW-trending fault is 1.1236. It shows that the NW-trending fault plays a controlling role in the rock burst of Junde Coal Mine, while the NE-trending fault has an important influence on the rock burst. The analytic hierarchy process is used to de-termine the weight of each influencing factor, and the GIS software is used to normalize and superimpose it. The study area is di-vided into four regions. In the past, rock burst accidents mostly occurred in dangerous areas, which is consistent with the actual situation.The research method provides a scientific basis for the prevention and control of rock burst disaster.
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