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Estimation of Bulk Density, Recovery Tests and Mineralogical Analysis of Iron Ore Mine at Obulapuram Village, Anantapur District, Andhra Pradesh

机译:Abulapuram村,Anantapur区,安德拉邦山脉坝矿矿山批量密度,恢复试验及矿物学分析

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The iron ore formation belongs to Precambrian, Dharwarian age. The lithological formations consists of Sedimentary and metamorphic rocks represented by Quartzite, shale, slate and phylites and iron ore occurring in from the mainly massive and fairable brown color hematite type presented. Source rock belongs to Banded hematite quartzite (BHQ) formation. The main Iron ore had been initially worked as open pit method of mining. The Hematite ore concentration mainly along the ferruginous shale and at some places pyrites are encountered. The recovery percentage of iron ore samples varied from 58.50%, 63% and 61%, the average being the float ore recovery is around 43%. The float ore occurs to a limited thickness of 1m and the workings are being carried out forming single bench to a maximum height of 3m from the surface. The results of the bulk density determined in the field for iron ore shown are 2.98 to 3.03. The average bulk density for float ore can be taken as 2.51. In the case of Iron ore the average works out to be 2.88.
机译:铁矿石形成属于Precambrian,Dharwarian时代。岩性形成由石英岩,页岩,石板和文学和手池和铁矿石以及来自主要且公式可公平的棕色赤岩型发生的铁矿石组成的沉积和变质岩。源岩属于带状赤铁矿石英岩(BHQ)形成。主要的铁矿石已最初是露天采矿方法。静脉岩矿石浓度主要沿着铁蝇和某些地方捕获。铁矿石样品的恢复百分比从58.50%,63%和61%变化,平均浮法矿石回收率约为43%。浮子矿体发生在1M的有限厚度上,并且在从表面上形成单个台阶至最大高度为3m。所示铁矿石现场测定的堆积密度的结果为2.98至3.03。浮法矿石的平均堆积密度可作为2.51取。在铁矿石的情况下,平均值为2.88。

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