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New Ore Types from the Caue Banded Iron Formation, Quadrilatero Ferrifero, Minas Gerais, Brazil - Responses to the Growing Demand

机译:来自Caue带状铁形成的新矿石类型,Quadrilatero Ferrififero,Minas Gerais,Brazil - 对需求不断增长的回应

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The mining district of the Quadrilatero Ferrifero (QF) in southeastern Brazil contributes to 70 per cent of the Brazilian iron ore production, which reached 370 Mt in 2010. Traditionally, four iron ore types were mined in the QF region: 1. soft haematite, 2. hard haematite, 3. friable 'itabirite' (the Brazilian name for metamorphosed banded iron formation), and 4. canga (an indurated iron-rich crust). With the exception of the hard haematite, these categories derive from supergene enrichment of the Paleoproterozoic Caue Itabirite. High current iron ore demand means that the QF high grade supergene ores will be depleted in a few decades. Consequently, several mining projects are being developed to exploit unenriched, fresh itabirite. Among them, the Mineragao Usiminas Serra Azul project in northwestern QF is one of the most advanced. Four major itabirite types occur in the QF region: 1. siliceous (or standard), 2. dolomitic, 3. amphibolitic, and 4. magnetitic. The dominant type in Serra Azul region is a fresh siliceous itabirite, composed essentially of haematite, martite and quartz that averages 36 per cent Fe (51.5 per cent Fe_2O_3) and 47 per cent SiO_2. The second type, the magnetitic itabirite, consisting of magnetite, martite, grunerite-cummingtonite, quartz, dolomite, stilpnomelane, and subordinate haematite, is typically a strongly magnetic greenish banded iron formation with the iron grade varying between 25 and 35 per cent. Chemically, it differs from the siliceous itabirite due to the relatively high CaO, MgO and, consequently, high LOI contents. Together with supergene ores, fresh itabirites have been included in the ore reserves of the Serra Azul project. We anticipate that all the four types of fresh itabirite will be incorporated as ore in the QF region, causing a huge increase on the iron ore resources of the district, and representing enormous environmental and technological challenges for the local iron ore industry.
机译:巴西东南部的Quadrilatero Ferrifero(QF)的矿区占巴西铁矿石生产的70%,2010年达到了370吨。传统上,QF地区开采了四种铁矿石类型:1。软血清矿, 2.硬水,3.易碎的'itabirite'(巴西名称变形带状铁形成),4. Canga(富含铁富含铁的外壳)。除了硬氧气的外,这些类别来自古普罗佐奇的超级富集浮石itabirite。高电流铁矿石需求意味着QF高级超级矿石将在几十年内耗尽。因此,正在开发几个采矿项目来利用未经内容,新鲜的itabirite。其中,西北QF的米塔哥·勒维纳斯塞拉阿祖尔项目是最先进的。在QF区域发生四种主要itabirite类型:1。硅质(或标准),2.白云岩,3.锥形岩和4.磁铁。 Serra Azul地区的主导类型是一种新鲜的硅灰石,基本上由哈内矿石,军子和石英组成,平均36%的Fe(51.5%Fe_2O_3)和47%的SiO_2。第二种类型,由磁铁矿,马丁基,Grunerite-Cummington,石英,白云石,斯蒂替纳米甲烷和从属血液矿石组成的磁性烟灰石通常是一种强磁性的绿色带状铁形成,铁级不同于25%至35%。在化学上,由于相对高的CaO,MgO,并且因此,高LOI含量,它与硅质陶瓷不同。与Supergene ORES一起,新鲜的itabirites已包含在Serra Azul项目的矿石储备中。我们预计所有四种新鲜的itabirite将在QF地区的矿石中纳入矿石,导致该区的铁矿石资源巨大增加,并为当地铁矿石行业代表巨大的环境和技术挑战。

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