Iron and Manganese Mineralization Associated with Archean Greenstone Belt in Joda-Noamundi Sector, Odisha, East Indian Shield

R. Ghosh, D. Chakraborty, M. Halder, T. K. Baidya
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引用次数: 1

Abstract

Iron and manganese mineralization in the Joda-Noamundi sector is associated with Banded Iron Formation of the Archean Iron Ore Group of rocks (3.5-3.0 Ga).Both Mn and Fe mineralization is stratiform and stratabound. In the Noamundi basin the estimated reserve of Fe and Mn -ores are 3.3 Gt and 130 Mt respectively. The Fe and Mn-mineralization are also genetically related to each other. A detailed petrology, mineralogy and mineral chemistry of the ores show their evolution with respect to different tectonic phases. During the first phase of deformation and metamorphism Fe-protolith generated magnetite and Mn-protolth generated bixbyite, hausmannite, jacobsite and braunite. During second phase martitized magnetite and hematite in Fe-ore and hollandite, psilomelane and pyrolusite in Mn-ore were generated. During supergene events low temperature higher oxide minerals were generated from the metamorphic and hydrothermal Fe and Mn –ore minerals. The stratigraphic status of the Fe- and Mn- ores with respect to crustal evolution has been established
东印度地盾奥里萨邦Joda-Noamundi板块太古宙绿岩带铁锰成矿作用
Joda-Noamundi段的铁、锰成矿作用与太古代铁矿群(3.5-3.0 Ga)的条带状铁组有关。锰、铁成矿均为层状和层控。Noamundi盆地铁、锰矿估计储量分别为3.3亿吨和1.3亿吨。铁矿化和锰矿化也有遗传关系。详细的岩石学、矿物学和矿物化学资料显示了矿石在不同构造阶段的演化过程。在第一阶段的变形变质作用中,铁原岩生成磁铁矿,锰原岩生成辉长石、豪氏辉长石、雅可辉长石和布朗辉长石。在第二阶段,铁矿和荷兰矿中的磁铁矿和赤铁矿被磁化,锰矿中的软锰矿和软锰矿被生成。在表生事件中,由变质和热液形成的铁、锰矿物形成低温高氧化矿物。确定了铁、锰矿在地壳演化中的地层地位
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