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Occurrence of Manganese Ore Deposits and Their Mineralogy in Vizianagaram-Visakhapatnam Manganese Ores Belt (Andhra Pradesh) India

机译:印度Vizianagaram-Visakhapatnam锰矿带(安得拉邦)锰矿床的赋存及其矿物学

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The Manganese deposits of Andhra Pradesh are associated with a thick sequence of Precambrian rocks, belonging to Khondalite and Charnockite groups of Dharwar Supergroup that forms part of 2500 to 3000 m.y. old Eastern Ghat complex of India. The study area is the Manganese deposits of Vizianagram-Visakhapatnam Manganese Belt of Andhra Pradesh. The study area lies about 150 km NE of Visakhapatnam between 18°12′N - 18°30′N and 83°20′E - 83°45′E. The mineralization of Manganese ores is confined to different rock types, belonging to both Khondalite and Charnockite groups, where they are dispersed throughout the country rocks as small lenses, pockets, veins and irregular bodies of varying dimensions. Quartz, garnet, clay, limonite and apatite are the common gangue minerals in the Manganese ores. The presence of quartz, garnet and apatite brings down the grade of the ore. Ferruginous laterite and ochre generally work as capping of the Manganese deposits. The various Manganese ore minerals present in these deposits are indentified as 1) Primary minerals-braunite, bixbyite, vredenburgite, jacobsite and hausmannite, 2) secondary minerals-psilomelane, cryptomelane, hollandite, pyrolusite and wad. The primary ore minerals are considered to be syngenetic and regionally metamorphosed while, the associated secondary ore minerals are formed due to alteration of the primary ores.
机译:安得拉邦(Andhra Pradesh)的锰矿床与厚厚的前寒武纪岩层有关,属于达哈尔超级群的本田岩和夏诺克岩群,构成了2500至3000 m.y的一部分。印度的老东高止山脉情结。研究区域是安得拉邦的Vizianagram-Visakhapatnam锰矿带的锰矿床。研究区域位于维沙卡帕特南(Visakhapatnam)东北约150公里,介于18°12′N-18°30′N和83°20′E-83°45′E之间。锰矿石的矿化仅限于不同的岩石类型,属于高棉岩和夏诺克岩,它们分散在整个国家的岩石中,如小晶状体,袋状,脉状和大小不规则的物体。石英,石榴石,粘土,褐铁矿和磷灰石是锰矿石中常见的脉石矿物。石英,石榴石和磷灰石的存在降低了矿石的品位。铁质红土和o石通常用作锰矿床的封盖。这些矿床中存在的各种锰矿石矿物鉴定为:1)初级矿物-褐铁矿,方铁矿,褐铁矿,褐铁矿和菱锰矿,2)次级矿物-倍氯黑ane石,隐锰矿,hol石,黄铁矿和一团。原矿矿物被认为是同质的,并且是区域性的变质,而相关的次生矿物质是由于原矿的改变而形成的。

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