首页> 外文会议>International Mining Geology Conference >Susceptibility and Gamma-Gamma Probe Measurements in Boreholes for Ore Boundary Determinations in LKAB's Iron Ore Mine in Malmberget, Northern Sweden
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Susceptibility and Gamma-Gamma Probe Measurements in Boreholes for Ore Boundary Determinations in LKAB's Iron Ore Mine in Malmberget, Northern Sweden

机译:瑞典北部马尔曼特尔北部LKAB铁矿石矿石边界测定的易感性和γ-gamma探针测量

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LKAB operates two underground mines in Kiruna and Malmberget, Sweden. Blast furnace pellet is the main product and makes up 70 per cent of total production. The orebodies are hosted by 1910 - 1860 Ma old volcanic rocks. The host rocks and the ores were affected by the Svecokarelian orogeny for 1890 - 1860 Ma ago. The deposit belongs to the Kiruna type apatite-rich iron ore. Magnetite is the main ore mineral but haematite is the dominant ore mineral in some orebodies in the western part of the deposit. Large-scale sublevel caving is the dominant mining method. Three main haulage levels are in operation at present. The ore boundaries and quality can be detected by geophysical logging resulting in reduced waste dilution and subsequent grade reduction. The susceptibility measurements have been used in the magnetite ore since 1991 and gamma-gamma measurements in the haematite ore since 1998. The mining scale has increased during the last 20 years but diamond drilling has remained at approximately 18 000 drilling metres per year. Uncertainties in the ore constructions can lead to unexpected cost increases, ore loss and dilution. The ore boundaries are evaluated with percussion drill holes using in-hole geophysics to achieve satisfactory geological knowledge. The probes are calibrated in all currently mined orebodies. The correlation between core sample assays and measured susceptibility and gamma-gamma values is strong. The cost to determine the ore boundary by percussion drilling with in-hole geophysics is two-thirds lower, and productivity is six times higher compared to diamond drilling. The measurements are made by geotechnicians and the interpretations by a geologist. The results are transferred to a database and presented three dimensionally as holes with iron grade intervals on mine maps. The interpreted holes are used by the geologist in various ways in the geological modelling. Layout planning uses the measurements as a tool to place the drifts at the correct distance from the ore contact especially in the longitudinal sublevel caving and the production hole planning to optimise the final length of the cross-cuts and drifts for best ore recovery.
机译:LKAB工作在基律纳和马尔姆贝里耶,瑞典有两家地下矿井。高炉粒料是主要产品和构成70%的总生产的百分之。矿体由主办1910 - 1860粒麻古火山岩。 1860马前 - 主机岩石和矿石是为1890年受Svecokarelian造山运动。该矿床属于基律纳型丰富磷灰石铁矿石。磁铁矿的主要矿石矿物,但赤铁矿是在矿床西部一些矿体的主要矿石矿物。大型分段崩落是主要的开采方法。三个主要的运输水平在操作目前。矿石边界和质量可以通过导致降低废物稀释和随后的级降低地球物理测井来检测。磁化率测量已在磁铁矿自1991年以来一直使用,在赤铁矿矿石的γ-γ的测量,因为1998年的开采规模在过去20年增加,但金刚石钻探一直保持在每年约18 000钻米。矿石结构的不确定性可能会导致意外成本的增加,矿石损失贫。矿石边界与使用孔地球物理达到满意的地质知识冲击钻的孔进行评价。探针被校准在所有当前开采矿体。岩心样品测定和测量的敏感性和γ-γ值之间的相关性强。以确定由冲击钻井矿石边界与孔地球物理成本三分之二降低,并且生产率是高六倍相比金刚石钻孔。测量是通过geotechnicians和解释由地质学家提出。将结果传送到一个数据库,并呈现三维如铁品位间隔孔上矿映射。该解释的孔被在地质建模各种方式地质学家使用。布局规划使用测量值作为放置在漂移从矿石接触特别是在纵向分段崩落和生产规划孔的正确距离,以优化横切口和漂移的最佳矿石回收最终长度的工具。

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