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

Received: 4 May 2015     Accepted: 6 July 2015     Published: 29 July 2015
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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

Published in Earth Sciences (Volume 4, Issue 4-1)

This article belongs to the Special Issue Archean Metallogeny and Crustal Evolution

DOI 10.11648/j.earth.s.2015040401.13
Page(s) 31-39
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2015. Published by Science Publishing Group

Keywords

Archean, Fe-Mn-ores, Iron Ore Group, East Indian Shield

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Cite This Article
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    R. Ghosh, D. Chakraborty, M. Halder, T. K. Baidya. (2015). Iron and Manganese Mineralization Associated with Archean Greenstone Belt in Joda-Noamundi Sector, Odisha, East Indian Shield. Earth Sciences, 4(4-1), 31-39. https://doi.org/10.11648/j.earth.s.2015040401.13

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    ACS Style

    R. Ghosh; D. Chakraborty; M. Halder; T. K. Baidya. Iron and Manganese Mineralization Associated with Archean Greenstone Belt in Joda-Noamundi Sector, Odisha, East Indian Shield. Earth Sci. 2015, 4(4-1), 31-39. doi: 10.11648/j.earth.s.2015040401.13

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    AMA Style

    R. Ghosh, D. Chakraborty, M. Halder, T. K. Baidya. Iron and Manganese Mineralization Associated with Archean Greenstone Belt in Joda-Noamundi Sector, Odisha, East Indian Shield. Earth Sci. 2015;4(4-1):31-39. doi: 10.11648/j.earth.s.2015040401.13

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  • @article{10.11648/j.earth.s.2015040401.13,
      author = {R. Ghosh and D. Chakraborty and M. Halder and T. K. Baidya},
      title = {Iron and Manganese Mineralization Associated with Archean Greenstone Belt in Joda-Noamundi Sector, Odisha, East Indian Shield},
      journal = {Earth Sciences},
      volume = {4},
      number = {4-1},
      pages = {31-39},
      doi = {10.11648/j.earth.s.2015040401.13},
      url = {https://doi.org/10.11648/j.earth.s.2015040401.13},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.s.2015040401.13},
      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},
     year = {2015}
    }
    

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  • TY  - JOUR
    T1  - Iron and Manganese Mineralization Associated with Archean Greenstone Belt in Joda-Noamundi Sector, Odisha, East Indian Shield
    AU  - R. Ghosh
    AU  - D. Chakraborty
    AU  - M. Halder
    AU  - T. K. Baidya
    Y1  - 2015/07/29
    PY  - 2015
    N1  - https://doi.org/10.11648/j.earth.s.2015040401.13
    DO  - 10.11648/j.earth.s.2015040401.13
    T2  - Earth Sciences
    JF  - Earth Sciences
    JO  - Earth Sciences
    SP  - 31
    EP  - 39
    PB  - Science Publishing Group
    SN  - 2328-5982
    UR  - https://doi.org/10.11648/j.earth.s.2015040401.13
    AB  - 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
    VL  - 4
    IS  - 4-1
    ER  - 

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Author Information
  • Department of Geological Sciences, Jadavpur University, Kolkata-700032, India

  • Department of Geological Sciences, Jadavpur University, Kolkata-700032, India

  • Department of Geological Sciences, Jadavpur University, Kolkata-700032, India

  • Department of Geological Sciences, Jadavpur University, Kolkata-700032, India

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