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首页> 外文期刊>Journal of the Geological Society of India >Vanadium bearing titaniferous magnetite ore bodies of Ganjang, Karbi-Anglong District, Northeastern India
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Vanadium bearing titaniferous magnetite ore bodies of Ganjang, Karbi-Anglong District, Northeastern India

机译:印度东北Karbi-Anglong区Ganjang的含钒钛铁矿磁铁矿体

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摘要

A new occurrence of (syenite-hosted) Vanadium bearing titaniferous magnetite ore body has been reported from Ganjang (26°09'35" N: 93°20' E), Karbi-Anglong, Northeastern India. The magnetite ore bodies have lumpy and sporadic occurrences within the host syenite pluton intrusive into gneissic country rocks. Ore microscopic studies reveal that magnetite is often associated with haematite and ilmenite depicting different textural patterns. Critical consideration of several elemental patterns suggests magmatic differentiation to be main ore-forming process. The ore body is suggested to have been formed as late stage segregation from a differentiating alkaline magma in a fluid enriched milieu.
机译:据报道,印度东北部喀比昂隆的甘姜(26°09'35“ N:93°20'E)出现了一种新的(含硒的)含钒钛磁铁矿矿体。该磁铁矿体呈块状和块状。块状正长岩侵入岩体中的片麻岩乡村岩石中,矿石微观研究表明,磁铁矿通常与描绘出不同组织形态的赤铁矿和钛铁矿有关,对几种元素形态的批判性考虑表明,岩浆分异作用是成矿的主要过程。建议在富液的环境中,由于分化的碱性岩浆的后期分离而形成了主体。

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