印度奥里萨邦Bonai-Keonjhar带低品位硅质锰矿的矿石岩石学:矿物结构对其选矿的影响

Mishra Subrat, Mohapatra Birendra Kumar, Dash Nilima, Rao Danda Srinivas
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引用次数: 10

摘要

印度奥里萨邦Bonai-Keonjhar带铁矿群中的低品位硅质锰矿石多产于剪切带。研究了三个不同矿山的硅质锰矿样品的矿石特征,即Shankar (Barbil OMC租赁区),Sone-Patuli (Patmunda, OMC租赁区)和Musaghar (Roida, OMDC租赁区)。这些硅质锰矿石主要有三种类型:(i)海绵状粒状;(2) massive-mosaic;(三)硬糜棱化。海绵状颗粒型含粒状、糖状石英,主要锰矿物为软锰矿。第二类含结晶良好的石英和隐黑岩,第三类含细晶石英(糜棱岩)和罗曼辉石。三种矿石均在相似条件下进行了物理选矿。采用了重力和磁选两种技术。矿石的矿物结构与使用这些物理技术的选矿程度有关。3种矿石中,只有海绵状颗粒型对改造反应较好。锰含量由22%提高到44%,产率28%,回收率49%。海绵状颗粒样对选矿的良好响应可能是由于软锰矿的大自面体晶体和糖晶石英的易碎性。研究揭示了矿物结构对低品位矿石特别是硅质锰矿选矿的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ore petrography of low-grade siliceous manganese ores from the Bonai-Keonjhar belt, Orissa, India: The influence of mineral-fabric on their beneficiation

Low grade siliceous manganese ores from the iron ore group of the Bonai-Keonjhar belt, Orissa, India are found mostly in shear zones. The ore characteristics of siliceous manganese ore samples from three different mines, viz. the Shankar (Barbil OMC lease hold area), the Sone-Patuli (Patmunda, OMM lease hold area), and the Musaghar (Roida, OMDC lease hold area), were studied. These siliceous manganese ores are of three types, respectively: (i) spongy-granular; (ii) massive-mosaic; and (iii) hard-mylonitized. The spongy-granular type contains granular, saccharoidal quartz and the major manganese mineral present is pyrolusite. The second type contains well crystallized quartz and cryptomelane, while the third has cherty, fine grained quartz (mylonite) along with romanechite. All three ores were subjected to physical beneficiation under similar conditions. Both gravity and magnetic separation techniques were employed. The mineral-fabric of the ores has been correlated to the extent of their beneficiation using these physical techniques. Of these three ores only the spongy-granular type responded well to upgrading. The feed with 22% Mn content could be upgraded to 44% with a 28% yield and a 49% recovery. The good response to beneficiation of the spongy-granular sample could be due to the large euhedral crystals of pyrolusite and the friable nature of the saccharoidal quartz. This study reveals the influence of mineral-fabric on beneficiation of low grade ore, siliceous Mn ore in particular.

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