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Metamorphosed Banded Iron Formation of Gorumahisani-Sulaipat-Badampahar belt, in Precambrian Iron Ore Group, Singhbhum Craton, India: ore petrography, micro-chemical and genetic studies

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Abstract

The metamorphosed Banded Iron Formation (BIF) of Gorumahisani-Sulaipat-Badampahar (GSB) belt in Precambrian Iron Ore Group, Singhbhum Craton, is well known in the mineral map of India. Detailed characteristics of iron ore and iron-containing rocks in BIF have been investigated at different mine profiles and results are interpreted in terms of their genetic evolution. The BIF constitutes four different facies such as carbonate, silicate, oxide and sulphide in variable proportion. The carbonate facies (Fe-Mn-Mg-Ca) appear as relicts within the oxide facies. The silicate facies includes Co-bearing cummingtonite-grunerite solid solution and quartz. The oxide facies is dominated by magnetite but markedly martitised/goethitised. The protolith of these facies of BIF ore envisioned as carbonate-containing mud originated from a submarine exhalative source, with high concentrations of Fe and Si and lower contents of Mn, Co, Mg and Ca which coprecipitated in an oxidised mixed hydrothermal-marine environment. Subsequently, this has undergone both submarine weathering and metamorphic changes in their evolution. During submarine weathering, carbonates (in Fe-Mn-Mg-Ca solid solution), sheet silicates (greenalite) and quartz were formed. At the outset of regional metamorphic episode, cummingtonite-grunerite and magnetite were developed. Magnetite formed at the expense of carbonate due to decarbonation and was later martitised to haematite and goethitised under post-metamorphic and supergene conditions respectively. With an increasing grade of metamorphism, greenalite transformed to grunerite-cummingtonite solid solution while quartz showed recrystallisation and grain size enlargement.

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References

  • Acharya S, Amstutz GC, Sarangi SK (1982) Diagenetic crystallisation and migration in the banded iron formations of Orissa, India. In G.C.Amstutz, A.El Goresy, G. Frenzel, C. Kluth, G. Moh, A. Wauschkuhn and R.A. Zimmermann(ed) Ore Genesis The State of the Art, Springer-Verlag, Berlin, pp 442–450

  • Banerji AK (1974) On the stratigraphy and tectonic history of iron ore bearing and associated rocks of Singhbhum and adjoining areas of Bihar and Orissa. Jour Geol Soc India 15:150–157

    Google Scholar 

  • Berge JW, Johanssen K, Jack J (1977) Geology and origin of the hematite ores of the Nimba Range, Liberia Econ. Geol. 72:582–607

    Google Scholar 

  • Beukes NJ, Gutzme J (2008) Origin and paleoenvironmental significance of major iron formations at the Archean-Paleoprotorozoic boundary. Econ Geol Rev 15:5–47

    Google Scholar 

  • Beukes NJ, Mukhopadhyay J, Gutzmer JG (2008) Genesis of high grade iron ores of the Archean Iron Ore Group around Noamundi. Econ Geol 103:365–386

    Article  Google Scholar 

  • Beura D (2017) Diagenetic behavior of Iron Formation of Badampahar-Gorumahisani-Suleipat belt. Vistas in Geological Research, Special publication in Geology (15), P. G. Department of Geology, Utkal University, Bhubaneswar: 12–19

  • Beura D, Singh P, Satpathy B, Behera S, Nanda SK (2016) Field relationship among the three iron Ore Groups of Iron Ore Supergroup encircling the North Odisha Iron Ore Craton, India: a comparison study. Journal of Geosciences and Geomatics 4(3):53–60

    Google Scholar 

  • Bhattacharya HN, Chakraborty I, Ghosh KK (2007) Geochemistry of some banded iron formations of the Archean supracrustals, Jharkhand–Orissa region. India J Earth System Science 116(3):245–259

    Article  Google Scholar 

  • Bowen NL, Schairer JF (1935) Grunerite from Rockport, Massachusetts, and a series of synthetic fluor-amphiboles. Am Mineral 20:547

    Google Scholar 

  • Chakraborty KL (1958) Metamorphism of the banded Iron-formation of Badampahar, Mayurbhanj, India and the origin of the cummingtonite-magnetite rock. Proc Nat Inst Sci of India 24A:386–391

    Google Scholar 

  • Chakraborty KL, Majumder T (2002) Some important aspects of the banded iron formation (BIF) of eastern Indian shield (Jharkhand and Orissa). Indian J Geol 74(1–4):37–47

    Google Scholar 

  • Chakraborty KL, Taron PB (1968) Thermal metamorphism of the banded iron formation of Orissa. India Geol Soc Am Bull 79:365–374

    Article  Google Scholar 

  • Doody A (2006) Petrology of banded iron formation and phyllite in the standard creek contact aureole, southern gravelly mountains. 19th Annual Keck Symp:177–182

  • Dunn JA (1935) The origin of iron ores in Singhbhum, India. Econ Geol 30:643–654

    Article  Google Scholar 

  • Dunn JA (1937) The mineral deposits of Eastern Singhbhum and surrounding areas: Mem. Geol Survey India 69:211–213

    Google Scholar 

  • Eichler J (1976) Origin of the Precambrian banded iron-formation. Handbook of Stratiform and Stratabound-Ore Deposits. Elsevier, Amsterdam, 7, pp 201

  • Eugster H P (1959) Reduction and oxidation in metamorphism: in researches in Geochemistry (Ed. P.H. Abelson), 397–426

  • Floran RJ, Papike JJ (1978) Mineralogy and petrology of the gunflint iron formation, Minnesota and Ontario: correlation of compositional and assemblage variations at low to moderate grade. Journal of Petrology 19:215–288

    Article  Google Scholar 

  • French BM (1968) Progressive contact metamorphism of the Biwabik iron-formation, Mesabi range, Minnesota. Minnesota Geol Survey Bull 45:103

    Google Scholar 

  • Goode ADT, Hall WDM, Bunting JA (1983) The Nabberu basin of Western Australia. In: Trendall AF, Morris RC (eds) Iron-formation facts and problems, Developments in Precambrian geology, vol 6. Elsevier, New York, pp 295–323

    Chapter  Google Scholar 

  • Haase CS (1982) Metamorphic petrology of the Negaunee iron formation, Marquette District, northern Michigan: mineralogy, metamorphic reactions, and phase equilibria. Econ Geol 77:60–81

    Article  Google Scholar 

  • Jaffe HW, Groeneveld Meijer WOJ, Selchow DH (1961) Manganoan Cummingtonite from nsuta. Ghana, American Mineralogist 46:64–653

    Google Scholar 

  • James HL (1955) Zones of regional metamorphism in the Precambrian of northern Michigan. Geol Soc Am Bull 66:1455–1488

    Article  Google Scholar 

  • Jirsa MA, Miller JD Jr, Morey GB (2008) Geology of the Biwabik iron formation and Duluth complex. International Symposium on the Health Hazard Evaluation of Fibrous Particles Associated with Taconite and the Adjacent Duluth Complex - Taconite Symposium 52:5–10

    Google Scholar 

  • Jones HC (1934) The iron ores deposits of Bihar and Orissa. Geol Surv India Memoir 63:375

    Google Scholar 

  • Kalliokoski J (1965) The metamorphosed iron ore of EI Pao. Venezuela Econ Geol 60:100–166

    Article  Google Scholar 

  • Klein C Jr (1964) Cummingtonite-Grunerite series: a chemical, optical and X-ray study. Am Mineral 49:963–982

    Google Scholar 

  • Klein C Jr (1973) Changes in mineral assemblages with metamorphism of some banded Precambrian iron-formations. Econ Geol 68:1075–1088

    Article  Google Scholar 

  • Klein Jr C (1983). Diagenesis and metamorphism of Precambrian banded iron-formation. In: a.F. Tre-all and R.C. Morris (Eds.). Iron-formation: facts and problems. Elsevier, 417-469

  • Mel’nik Y P (1982) Precambrian banded iron-formations, physico-chemical condition of formation, Elsevier, 310

  • Misra S (2006) Precambrian chronostratigraphic growth of Singhbhum-Orissa craton, eastern Indian shield: an alternative model. Journal Geological Society of India 67:356–378

    Google Scholar 

  • Miyano T, Beukes NJ (1997) Mineralogy and petrology of the contact metamorphosed amphibole asbestos-bearing Penge Iron Formation, Eastern Transvaal. South Africa J Of Petrology 38(5):651–676

    Google Scholar 

  • Morgan R, Oberger B, Rosiere CA, Wirth R, Carvalho CM, Bellver-Baca AT (2013) The origin of coexitising carbonates in banded iron formations: a micro-mineralogical study of the 2.4 Ga Itabira Group, Brazil. Precambrian Res 224:491–511

    Article  Google Scholar 

  • Mücke A, Annor A (1993) Examples and genetic significance of the formation of iron oxides in the Nigerian Banded Iron-Formations. Mineral Deposita 28:136–145

    Article  Google Scholar 

  • Mukhopadhyay D (2001) The Archaean nucleus of Singhbhum: the present state of knowledge. Gondwana Res 4:307–318

    Article  Google Scholar 

  • Mukhopadhyay J, Gutzmer J, Beukes NJ, Hayashi KI (2008) Stratabound magnetite deposits from the eastern outcrop belt of the Archean Iron Ore Group, Singhbhum craton, India. Appl Earth Sci 117(4):175–186

    Article  Google Scholar 

  • Nayak PK, Mohapatra BK, Singh PP, Martha RK (2011) Cobalt-bearing grunerite in the metamorphosed banded iron formation in Orissa, India. Resour Geol 61(3):281–289

    Article  Google Scholar 

  • Quade H (1988) Natural and simulated (10.4) pole figures of polycrystalline hematite. Textures Microtextures 89:719–736

    Article  Google Scholar 

  • Richarz S (1927) Grunerite rocks of the Lake Superior Region and their origin. Journ. Geol. 35:690–707

    Article  Google Scholar 

  • Saha AK, Ghosh S, Dasgupta D, Mukhopadhyay K, Ray SL (1984) Studies on crustal evolution of the Singhbhum-Orissa Iron ore Craton. Monograph on crustal evolution. Indian jour. Earth Sci:1–74

  • Sarkar SC (2000) Crustal evolution and metallogeny in the eastern Indian Craton. Geological Survey of India Special publication no 55:169–194

    Google Scholar 

  • Warren HV (1931) An occurrence of grunerite at Pierrefitte, Hautes-Pyrenees. France Mineral Mag 22:477–481

    Google Scholar 

Download references

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Correspondence to Patitapaban Mishra.

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Nayak, P.K., Mishra, P., Mohapatra, B.K. et al. Metamorphosed Banded Iron Formation of Gorumahisani-Sulaipat-Badampahar belt, in Precambrian Iron Ore Group, Singhbhum Craton, India: ore petrography, micro-chemical and genetic studies. Arab J Geosci 13, 588 (2020). https://doi.org/10.1007/s12517-020-05580-8

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