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Engineering geology, ground surface movement and fissures induced by underground mining in the Jinchuan Nickel Mine

机译:金川镍矿地下开采引起的工程地质,地表运动和裂隙

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摘要

The Jinchuan Nickel Mine is the largest underground mine with cut-and-fill mining in China. In 1999, there appeared evident ground surface movement and many ground fissures in Jinchuan No. 2 Mine. Following an introduction to the engineering geology and mechanical properties of the rock mass in the Jinchuan mine areas, this paper reveals the features of the measured in situ stresses and puts emphasis on an analysis of the mechanism of surface movement and ground fissures induced by the underground mining with backfill. It is indicated that both the fault structures and the alteration contact zones are well developed as the dominant engineering- geological characteristics in the Jinchuan mine areas. The stress redistribution in surrounding rocks resulting from the mining, the low stiffness of the filling body, the existence of the void space and the influence of on-going mining activities is the main reason for the occurrence of surface movement and ground fissures.
机译:金川镍矿是中国最大的地下采矿场。 1999年,金川二号矿出现明显的地表运动和许多裂隙。在介绍了金川矿区岩体的工程地质和力学特性之后,本文揭示了实测应力的特征,并着重分析了地下引起的地表运动和地裂缝的机理。回填开采。结果表明,断层构造和蚀变接触带均发育良好,是金川矿区的主要工程地质特征。开采引起的围岩应力重新分布,填充体刚度低,空隙空间的存在以及持续开采活动的影响是发生地表运动和地裂缝的主要原因。

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