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Titaniferous Magnetite Deposits Associated with Archean Greenstone Belt in the East Indian Sheild

Received: 04 May 2015    Accepted: 07 May 2015    Published: 29 July 2015
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Abstract

In the East Indian Shield, occurrence of titaniferous magnetite deposits associated with the Archean Greenstone belt occur in Kumhardubi, Betjharan and Nuasahi areas of Odisha and Dublabera area of Jharkhand. The ore bodies comprise lenses, veins, bands and patches within gabbroic rocks. Petrogenetic studies have revealed the primary and secondary mineral constituents of the ores such as titanomagnetite, ilmenite, hematite, spinel, cobaltite, goethite, martite, rutile and silicate gangue minerals. Various crystallographic intergrowths are resulted from exsolution & oxidation at different temperatures during cooling of the sub-solidus magma. Chemical analyses show that the ore contains 10.35 -17.68 wt.% TiO2, 0.148 – 0.227 wt.% V2O3 and 32.75 – 67.39 wt.% Fe2O3. Different geochemical composition diagrams confirm their tholeiitic origin. The formation of the massive ore bodies is referred to late magmatic crystallization from tholeiitic magma followed by Fe-Ti enriched residual liquid injection within the host rocks. Syn to late formation of the magnetite ores along with gabbro-anorthositic intrusive with respect to the Archean Greenstone Belt of East Indian Shield is suggested

DOI 10.11648/j.earth.s.2015040401.12
Published in Earth Sciences (Volume 4, Issue 4-1, July 2015)

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

Page(s) 15-30
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), 2024. Published by Science Publishing Group

Keywords

Magnetite, Archean, Orthomagmatic, Greenstone

References
[1] Chakraborty, K.L. and Mallik, A.K., 1968: Mineralogy and temperature of formation of titaniferous magnetite ores associated with gabbro in the Moulabhanjaparbat area, Dhenkanal district, Orissa. Bull. Geol.Soc. India, 5, 134-137.
[2] Vasudev, V.N. and Srinivasan, R., 1979: Vanadium-bearing titaniferous magnetite deposits of Karnataka, India. Jour. Geol. Soc. India, 20, 170-178.
[3] Vidyashankar, H.V. and Govindaiah, S., 2009: Ore petrology of the V-Ti magnetite (lodestone) layers of the Kurihundi area of Sargur Schist Belt, Dharwar Craton. Jour. Geol. Soc. India, 74, 58-68.
[4] Subba Rao, D.V., Basu, E.V.S.S.K., Balaram, V. and Vidyasagar, G., 2014: Geochemical Study of the Ultramafic-Mafic Plutonic and Volcanic Suites of the Nuggihalli Schist Belt, Western Dharwar Craton. Jour. Geol. Soc. India, Spec. Publ. no. 2, 107-126.
[5] Saha, A.K.. 1988: Some aspects of the crustal growth of the Singhbhum-Orissa Iron Ore craton, eastern India. Ind. J. Geol. 60(4), 270-278.
[6] Auge, T., Cocherie, A., Genna, A., Armstrong, R., Guerrot, C., Mukherjee, M.M. and Patra, R.N., 2003: Age of the Baula PGE mineralization (Orissa India) and its implications concerning the Singhbhum Archean Nucleus. Precambrian Res., 121, 85-101.
[7] Iyengar, S.V.P. and Alwar, M.A., 1965: The Dhanjori eugeosyncline and its bearing on the stratigraphy of the Singhbhum, Keonjhar and Mayurbhanj districts. D.N. Wadia Commen. Vol., Geol. Min. Met Soc. India. 138-162.
[8] Shackleton, R.M., 1995: Tectonic evolution of greenstone belts. From Coward, M.P. and Ries, A.C. (eds), 1995, Early Precambrian Processes, Geological Society, Special Publication No. 95, 53-65.
[9] Wilson, J.F., Nesbitt, R.W., and Fanning, C.M., 1995: Zircon geochronology of Archean felsic sequences in the Zimbabwe craton: a revision of greenstone stratigraphy and a model for crustal growth. From Coward, M.P. and Ries, A.C. (eds), Early Precambrian Processes, Geological Society, Special Publication No. 95, 109-126.
[10] Trendall, A.F., 1995: Paradigms for the Pilbara. From Coward, M.P. and Ries, A.C. (eds), Early Precambrian Processes, Geological Society, Special Publication No. 95, 127-142.
[11] Choukroune, P., Bouhallie, H. and Arndt, N.T., 1995: Soft lithosphere during periods of Archean crustal growth or crustal reworking. From Coward, M.P. and Ries, A.C. (eds), Early Precambrian Processes, Geological Society, Special Publication No. 95, 67-86.
[12] Myers, J.S., 1995: The generation and assembly of an Archean Supercontinent: evidence from the Yilgarncraton, Western Australia. From Coward, M.P. and Ries, A.C. (eds), Early Precambrian Processes, Geological Society, Special Publication No. 95, 143-154.
[13] Windley, B.F., 1977: The evolving Continents. Typeset in Linotron Times and printed by J. W. Arrowsmith Ltd. Bristol.
[14] Baidya, T.K., 2015: Archean Metallogeny and crustal evolution in the East Indian Shield. Jour. Earth Sciences, Special issue (accepted; to be published by July, 2015).
[15] Dunn, J.A. and Dey, A.K, 1937: Vanadium bearing titaniferous magnetite iron ores in Singhbhum and Mayurbhanj, India. Trans. Min. Geol. Inst. India, XI, pt.3, 117-194.
[16] Roy, S., 1956: Origin of the vanadium bearing titaniferous magnetite ores of Mayurbhanj, India. Proc. Nat. Inst. Sci. India, 22, 285-292.
[17] Chakraborty, K.L., Roy, J. and Majumder, T., 1988: Structures and textures of vanadium bearing titaniferous magnetite ores and their interpretation. Jour. Geol. Soc. India, 31, 305-313.
[18] Das, S.K., 1995: Petrology, mineralogy and geochemistry of gabbro-anorthosite suite of rocks and origin of the associated magnetite deposits of Amdabera-Hatichhar area, Mayurbhanj district, Orissa, India. Unpublished Ph.D. Thesis, Utkal University.
[19] Haggerty, S.E., 1976: Opaque mineral oxides in terrestrial igneous rocks. In ‘Review in Mineralogy - Oxide Minerals’. Mineralogical Society of America. ed. Douglas Rumble, 3, 101-299.
[20] Mohanty, J.K. and Paul, A.K., 2008: Fe-Ti-oxide Ore of the Mesoarchean Nuasahi Ultramafic-Mafic Complex, Orissa and its Utilization Potential. Jour. Geol. Soc. India, 72, 623-633.
[21] Das, S.K., 2014: Mineralogy and Ore Petrography of Vanadiferous Titaniferous Magnetite Ores of Mayurbhanj Basic Igneous Complex, Odisha. Jour. Geol. Soc. India Spec. Publ., 2, 127-137.
[22] Chevallier, R., Bolfa, J. and Mathieu, S., 1955: Titanomagnetites et ilmenites ferromagnetiques. Bull. Soc. Franc. Min. Crist., 78, 307-346.
[23] Frietsch, R., 1970: Sveriges Geol. Unders Arsbok, 64.
[24] Shaw, G.M., 1964: Interpretation geochimique des elements en Frances dans Les rockes Cristallina, Mason, Paris.
[25] Middlemost, E.A.K., 1985: Magmas and magmatic rocks. Longman, London.
[26] Cox, K.G., Bell, J.D. and Pankhurst, R.J., 1979: The interpretations of igneous rocks. George, Allen and Unwin, London.
[27] Miyashiro, A., 1974: Volcanic rock series in island arcs and active continental margins. Am. J. Sci. 274,321-55.
[28] Irvine, T.N. and Baragar, W.R.A., 1971: A guide to the chemical classification of the common volcanic rocks. Can. Earth Sci., 8, 523-548.
[29] Shervais, J.W., 1982: Ti-V plots and the petrogenesis of modern and ophiolitic lavas. Earth Planet Sci. Lett., 59, 101-113.
[30] Lister, G.F., 1966: the composition and origin of selected iron-titanium deposits. Econ. Geol., 61, 275-310.
[31] Reynolds, I.M., 1985b: The nature and origin of titaniferous magnetite-rich layers in the upper zone of the Bushveld complex; a review and synthesis. Econ. Geol., 80, 1089-1108.
[32] Zhou, M., Robinson, P.T., lesher, C.M., Keays, R.R., Zhang, C.J. and Malpas, J., 2005: Geochemisttry, Petrogenesis and Metallogenesis of the Panzhiua gabbroic layered intrusion and associated Fe-Ti-V oxide deposits, Sichuan province, SW China. Jour. Petrol., 46, 2253-2280.
[33] Charlier, B., Duchesne, J.C. and Auwera, J.V., 2006: Magma chamber processes in the Tellnes ilmenite deposit (Rogaland Anorthosite Province, SW Norway) and the formation of Fe-Ti ores in massif-type anorthosites. Chemical Geology, 234, 264-290.
[34] Das, S.K. and Mukherjee, S., 2001: Mineralogy geochemistry of V-Ti magnetite deposits of Mayurbhanj basic igneous complex, Orissa, Indian Mineralogist, 35, 134-150.
[35] Klemn, D.D., Henckel, J., Dehm, R., and Von Gruenewaldt, G., 1985: The geochemistry of titanomagnetite in magnetite layers and their host rocks of the Eastern Bushveld Complex. Econ. Geol., 80, 1075-1088.
[36] Cawthorn, R.G. and Ashwal, L.D., 2009: Origin of anorthosite and magnetite layers in the Bushveld complex: constrained by major element compositions of plagioclase. Jour. Petrol., 50, 1607-1637.
[37] Bateman, A.M., 1951: The formation of late magmatic oxide ores. Econ. Geol., 46, 404-426.
[38] Reynolds, I.M., 1985a: Contrasted mineralogy and textural relationships in the uppermost titaniferous magnetite layers of the Bushveld Complex in the Bierkraal area, north of Rustenburg. Econ. Geol., 80, 1089-1108.
[39] Irvine, T.N., 1975: Crystallization sequences in Muskox intrusion and other layered intrusions. 2. Origin of chromitite layers and similar deposits of other magmatic ores. Geochim.et Cosmochim. Acta, 39, 991-1020.
Author Information
  • Department of Geological Sciences, Jadavpur University, Kolkata: 700028, West Bengal, India

  • Department of Geological Sciences, Jadavpur University, Kolkata: 700028, West Bengal, India

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    Riya Mondal, Tapan Kr. Baidya. (2015). Titaniferous Magnetite Deposits Associated with Archean Greenstone Belt in the East Indian Sheild. Earth Sciences, 4(4-1), 15-30. https://doi.org/10.11648/j.earth.s.2015040401.12

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    Riya Mondal; Tapan Kr. Baidya. Titaniferous Magnetite Deposits Associated with Archean Greenstone Belt in the East Indian Sheild. Earth Sci. 2015, 4(4-1), 15-30. doi: 10.11648/j.earth.s.2015040401.12

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    AMA Style

    Riya Mondal, Tapan Kr. Baidya. Titaniferous Magnetite Deposits Associated with Archean Greenstone Belt in the East Indian Sheild. Earth Sci. 2015;4(4-1):15-30. doi: 10.11648/j.earth.s.2015040401.12

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  • @article{10.11648/j.earth.s.2015040401.12,
      author = {Riya Mondal and Tapan Kr. Baidya},
      title = {Titaniferous Magnetite Deposits Associated with Archean Greenstone Belt in the East Indian Sheild},
      journal = {Earth Sciences},
      volume = {4},
      number = {4-1},
      pages = {15-30},
      doi = {10.11648/j.earth.s.2015040401.12},
      url = {https://doi.org/10.11648/j.earth.s.2015040401.12},
      eprint = {https://download.sciencepg.com/pdf/10.11648.j.earth.s.2015040401.12},
      abstract = {In the East Indian Shield, occurrence of titaniferous magnetite deposits associated with the Archean Greenstone belt occur in Kumhardubi, Betjharan and Nuasahi areas of Odisha and Dublabera area of Jharkhand. The ore bodies comprise lenses, veins, bands and patches within gabbroic rocks. Petrogenetic studies have revealed the primary and secondary mineral constituents of the ores such as titanomagnetite, ilmenite, hematite, spinel, cobaltite, goethite, martite, rutile and silicate gangue minerals. Various crystallographic intergrowths are resulted from exsolution & oxidation at different temperatures during cooling of the sub-solidus magma. Chemical analyses show that the ore contains 10.35 -17.68 wt.% TiO2, 0.148 – 0.227 wt.% V2O3 and 32.75 – 67.39 wt.% Fe2O3. Different geochemical composition diagrams confirm their tholeiitic origin. The formation of the massive ore bodies is referred to late magmatic crystallization from tholeiitic magma followed by Fe-Ti enriched residual liquid injection within the host rocks. Syn to late formation of the magnetite ores along with gabbro-anorthositic intrusive with respect to the Archean Greenstone Belt of East Indian Shield is suggested},
     year = {2015}
    }
    

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  • TY  - JOUR
    T1  - Titaniferous Magnetite Deposits Associated with Archean Greenstone Belt in the East Indian Sheild
    AU  - Riya Mondal
    AU  - Tapan Kr. Baidya
    Y1  - 2015/07/29
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    N1  - https://doi.org/10.11648/j.earth.s.2015040401.12
    DO  - 10.11648/j.earth.s.2015040401.12
    T2  - Earth Sciences
    JF  - Earth Sciences
    JO  - Earth Sciences
    SP  - 15
    EP  - 30
    PB  - Science Publishing Group
    SN  - 2328-5982
    UR  - https://doi.org/10.11648/j.earth.s.2015040401.12
    AB  - In the East Indian Shield, occurrence of titaniferous magnetite deposits associated with the Archean Greenstone belt occur in Kumhardubi, Betjharan and Nuasahi areas of Odisha and Dublabera area of Jharkhand. The ore bodies comprise lenses, veins, bands and patches within gabbroic rocks. Petrogenetic studies have revealed the primary and secondary mineral constituents of the ores such as titanomagnetite, ilmenite, hematite, spinel, cobaltite, goethite, martite, rutile and silicate gangue minerals. Various crystallographic intergrowths are resulted from exsolution & oxidation at different temperatures during cooling of the sub-solidus magma. Chemical analyses show that the ore contains 10.35 -17.68 wt.% TiO2, 0.148 – 0.227 wt.% V2O3 and 32.75 – 67.39 wt.% Fe2O3. Different geochemical composition diagrams confirm their tholeiitic origin. The formation of the massive ore bodies is referred to late magmatic crystallization from tholeiitic magma followed by Fe-Ti enriched residual liquid injection within the host rocks. Syn to late formation of the magnetite ores along with gabbro-anorthositic intrusive with respect to the Archean Greenstone Belt of East Indian Shield is suggested
    VL  - 4
    IS  - 4-1
    ER  - 

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