首页> 外文会议>Eighth international mining geology conference 2011. >The Merlin Molybdenum Rhenium Deposit, Mt Isa Inlier – Two Years from Discovery to Development
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The Merlin Molybdenum Rhenium Deposit, Mt Isa Inlier – Two Years from Discovery to Development

机译:伊萨内里尔山梅林钼R矿床-从发现到开发的两年

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The Merlin project is situated 130 km south of Cloncurry in North West Queensland, Australia.rnIt is located within the Pre-Cambrian Mt Isa Inlier and is grouped within the Eastern Fold Belt.rnThe host rocks are metasedimentary rocks of the Proterozoic Kuridala and Staveley Formationsrnadjacent to the Mount Dore Granite.rnMerlin zone represents part of the Mount Dore polymetallic deposit containing copper, zinc,rnsilver, gold, lead, cobalt and most recently has been found to host molybdenum mineralisation.rnThis is intimately associated with economic grades of rhenium, a naturally occurring metal that isrnan important component of high temperature aircraft engines.rnThe host rock sequence is a 200 m thick zone of metasediments sandwiched between competentrngranite in the hanging wall and brittle quartzite in the foot wall. A distinct shear marks the contactrnbetween the granite and metasediments. The host rocks are comprised of three main rock types:rnblack shale, phyllite and altered banded calc-silicate.rnMineralisation dips to the east at approximately 45° in a package of fi ne grained pelites andrnbanded calc-silicates. The top 150 m of the sequence is typifi ed by black shale and phyllite. Thernlower 50 m is typifi ed by pink banded calc-silicate. The main molybdenite zone is located at andrnparallel to the pelite-calc-silicate contact. Down dip, the zone splits into two or three veins hostedrnby the calc-silicate rock suite and haloed by thin, steep dipping, stylolitic molybdenite veinlets.rnThe deposit was discovered in 2008 by routine infi ll reverse circulation sampling conductedrnfor the Mount Dore copper deposit. One hole penetrated below the main target Cu horizonrnand intersected visible molybdenite. During 2009 and 2010 a 50 × 50 m diamond drill patternrndelineated a total mineral resource of 6.7 Mt @ 1.3 per cent Mo, 23g/t Re, 0.3 per cent Cu (mostlyrnIndicated Mineral Resource with minor Inferred Mineral Resource). The resource has beenrnestimated using ordinary kriging within grade domains. Access to the deposit has commencedrnvia a decline and production through the nearby Osborne fl otation concentrator (70 km south) isrnexpected in 2012. All facilities and resources are fully owned and operated by Ivanhoe AustraliarnLimited, a public listed company on the Australian and Toronto stock exchanges.
机译:Merlin项目位于澳大利亚西北昆士兰州Cloncurry以南130公里处.rn它位于前寒武纪伊萨山脉内,在东部褶皱带内。默林区代表了多尔山多金属矿床的一部分,其中包含铜,锌,银,金,铅,钴,最近发现有钼矿化。这与economic的经济等级密切相关。天然金属是高温飞机发动机的重要组成部分。主岩层是夹在悬壁中的软锰矿和脚壁中的脆性石英岩之间的200 m厚的沉积物区域。明显的剪切标志着花岗岩和沉积物之间的接触。基质岩由三种主要岩石类型组成:黑色页岩,千枚岩和改变的带状钙硅酸盐。矿化作用在向东倾斜约45°,由细粒的钙质岩和带状钙硅酸盐组成。序列的前150 m以黑色页岩和橄榄石为代表。较低的50 m以粉红色带状钙硅酸盐为代表。主要的辉钼矿带位于与钙铁矿-钙-硅酸盐接触的平行处。向下倾斜时,该区域分为钙或硅酸盐岩套件所包围的两个或三个脉,并被稀薄的陡峭倾斜的针状辉钼矿脉晕着。2008年,该矿床是通过对多尔山铜矿床进行的常规反流取样而发现的。在主要目标铜层下方穿透了一个孔,并与可见辉钼矿相交。在2009年至2010年期间,一个50×50 m的金刚石钻探图样描绘了6.7 Mt的总矿产资源,其中Mo含量为1.3%,Re含量为23g / t,Cu含量为0.3%(主要是指示矿产资源,推断矿产资源较少)。在等级域内使用普通克里金法重新评估了资源。该矿床已开始减少,并于2012年通过附近的奥斯本浮选选矿厂(向南70公里)进行生产。所有设施和资源均由艾芬豪澳大利亚有限责任公司全资拥有和运营,艾芬豪澳大利亚有限责任公司是在澳大利亚和多伦多证券交易所上市的公司。

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