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Borehole periscope observations of rock fracturing ahead of the preconditioned mining faces in a deep level gold mine

机译:在深水平金矿的预处理采矿面前,岩石压裂的岩石潜望镜观察

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South Africa is one of the biggest gold producers in the world, with most of the gold mines found within the geological setting of the Witwatersrand basin. This basin hosts narrow and tabular reef deposits, which have been extensively mined for the past 100 years at shallow depths, using conventional mining techniques. Cur-rently, mining has progressed towards ultra-deep levels with the use of mechanized and conventional mining techniques. As mining depth increases, the stress levels ahead of the mining face increase rapidly, compromis-ing the stability of the tunnels and intersections of the excavations. These extreme high stresses increase the probability of face bursting. Owing to that, the face-perpendicular preconditioning blasting technique has been applied in order to redistribute the stress peak further into the solid region ahead of the mining face by elimi-nating the strain energy 'lock-ups' in the asperities of the pre-existing or mininginduced fractured. The objec-tives of the study were to identify the pattern of mining-induced fractures ahead of the preconditioned min-ing faces. To achieve the objectives of the study, borehole periscope observations and Ground Penetrating Radar were used to identify the fracture frequency ahead of the preconditioned mining faces. The results of the study have indicated that there were zones of fractured and un-fractured rock ahead of preconditioned mining faces, which were approximately 1m to 1.5m wide and continue as discrete entities for at least 14m parallel to the face and at least 7m to 8m vertically. Furthermore, analysis has shown that the zones of fracture do not form continuously as mining progresses. There is usually a solid zone of approximately 1m or more be-tween the fractured zones. The work presented in this paper is part of a Master of Science in Mining Engineer-ing by dissertation study at the University of the Witwatersrand, Johannesburg, and School of Mining Engi-neering, conducted by the first author.
机译:南非是世界上最大的黄金生产商之一,大部分金矿在Witwatersrand盆地的地质环境中发现。这种盆地寄出了狭窄的表格礁沉积物,使用传统的采矿技术在浅深度的过去100年中被广泛开采。在使用机械化和常规采矿技术的情况下,挖掘已经进展了超深层次。随着采矿深度的增加,采矿面前的应力水平迅速增加,折断隧道的稳定性和挖掘的交叉点。这些极高的应力增加了面部爆裂的概率。由此,应用了面垂直的预处理爆破技术,以便通过消除在预先预先的粗糙度中的应变能量“锁定”进一步将应力峰进一步进入挖掘面的固体区域。现有或突出的裂缝。该研究的Objec-tives是在预处理的矿物面前识别采矿诱导的骨折的模式。为了实现研究的目标,使用钻孔潜冲观测和地面穿透雷达来识别预先处理的采矿面前方的断裂频率。该研究的结果表明,预先处理的采矿面上有裂缝和未裂缝的岩石区的区域约为1米至1.5米,并继续与面部平行至少14米的离散实体,至少7米垂直8米。此外,分析表明,由于采矿的进展,骨折区域不会连续形成。通常存在大约1米或更多的裂缝区域的固体区。本文介绍的工作是通过第一作者进行的Witwatersrand大学的论文研究通过第一作者的矿业大学学报和矿业学院的矿业工程师学院学习硕士学位。

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