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Using existing data to improve the delineation of ore at the Olympic Dam Fe-oxide Cu-U-Au-Ag deposit

机译:利用现有数据改善奥林匹克坝Fe-oxide Cu-U-Au-Ag矿床上的矿石描绘

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An extensive suite of elements are routinely assayed on all resource drill core samples to assist in deposit scale resource definition, local mine scale delineation of ore zones, and ore characterisation for the planning and scheduling of mining and processing of ores at Olympic Dam. This paper discusses a deposit scale geochemical relation that can be used by mine geologists to find more high-grade ore at the local mine area scale at Olympic Dam. A 3D grade shell representing 0.8 per cent Cu was created for a mine area using drill hole assay data. This defined the geometry of the ore zone. The Cu-grade shell was then overlain onto the existing resource block model to evaluate the relationships between the Cu-grade shell, copper and other elements. The strongest correlation was between copper and manganese. The block model showed a dramatic decrease in the concentration of manganese just below the below the Cu-grade shell. Several drill holes that intersected the Cu-grade shell were selected to evaluate the copper manganese relation at the drill hole scale. As expected, the individual drill holes displayed a strong inverse relation between copper and manganese. A geochemical footwall was then modelled representing 0.1 wt per cent Mn. Using both the Cu- and Mn-grade shells, several drill holes were designed/drilled and all hit high-grade copper. For the vast majority of the deposit the inverse relation between copper and manganese is valid; however, in areas with intense chlorite alteration (related to amounts of mafic to ultramafic rocks) this relation is not as strong, due to increased manganese in the rock mass. Even though using the copper manganese relation as a drill targeting method was not always as reliable in a few small areas of the deposit, it demonstrates the value of using existing assay data integrated with the resource block model to discover local mine scale geochemical relationships which can be used to more effectively design drill holes to discover high-grade ore at Olympic Dam.
机译:在所有资源钻孔核心样本上常规测定一套广泛的元素,以协助存款规模资源定义,奥林匹克大坝采矿和矿石矿井的规划和调度的矿石规模划分,矿石表征。本文讨论了矿井地质学家可用于在奥林匹克大坝当地矿山面积秤中找到更多高档矿石的存款规模地球化学关系。使用钻孔测定数据为矿区创建代表0.8%Cu的3D级壳。这定义了矿石区域的几何形状。然后将Cu级外壳覆盖在现有的资源块模型上以评估Cu级壳,铜和其他元件之间的关系。最强的相关性是铜和锰之间。块模型表明,在Cu级壳以下的锰浓度下显着降低。选择几个与Cu级壳壳相交的钻孔以在钻孔尺度上评估铜锰关系。如预期的那样,个体钻孔呈现出铜和锰之间的强烈反向关系。然后模拟地球化学脚壁,其建模代表0.1wt%的Mn。使用Cu-and Mn级壳,设计/钻孔,所有钻孔都被设计/钻孔,并击中高级铜。对于绝大多数沉积物,铜和锰之间的反向关系是有效的;然而,由于岩体中的锰增加,在强烈的氯酸盐改变(与MAFIC的数量有关的母乳岩有关的情况下,这种关系并不是强烈的。尽管使用铜锰关系作为钻头靶向方法并不总是可靠的沉积物,但它展示了使用与资源块模型集成的现有测定数据的价值发现,以发现可以的本地矿山地球化学关系用于更有效地设计钻孔以在奥林匹克坝上发现高档矿石。

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