Volume 4, Issue 4-1, July 2015, Page: 1-14
Archean Metallogeny and Crustal Evolution in the East Indian Shield
Tapan Kumar Baidya, Department of Geological Sciences, Jadavpur University, Kolkata, India
Received: Mar. 20, 2015;       Accepted: Mar. 26, 2015;       Published: Jul. 29, 2015
DOI: 10.11648/j.earth.s.2015040401.11      View  6530      Downloads  217
Abstract
East Indian Shield bears the evidences of Archean metallogenic and crustal evolution like the other major shield areas of the world. The primordial continental crust in the form of more silicic bodies were floating like metallurgical slags over the hotter and denser ultramafic-mafic lithosphere (UM-ML) before 3800 Ma. Earliest sediments, now represented by the Older Metamorphic Group (OMG) , were deposited in small basins the basement of which was made of UM-ML containing rafts of primitive silicic bodies. Possibly the earliest greenstone rocks (some banded iron formation, associated high-Mg basalts and ultramafics) formed in the OMG with deformation and metamorphism continued upto about 3500 Ma. Partial melting of the lower amphibolitic crust due to underplating and asthenospheric sagging formed the tonalitic magma around 3500 Ma (Older Metamorphic Tonalitic Gneiss or OMTG) and subsequently Singhbhum Granite Type-A (Phase-I and Phase-II) around 3300 Ma both of which intruded the folded and metamorphosed OMG rocks. The major event of greenstone belt formation took place during 3500-3200 Ma both in the eastern part and in the western part of the Singhbhum granitic craton. The general trend of these two greenstone belts is NNE-SSW and they were the repositories of the Iron Ore Group (IOG) sediments, volcanics and ultrmafic-mafic rocks. The IOG rocks formed prolific mineralization of Fe,Mn,Cr,Ti,Cu,Ni,Au and platinum group elements(PGE). Multiple phases of tectonism and partial melting of crustal materials ultimately led to the formation of Singhbhun Granite Type-B (Phase-III) around 3100 Ma which later intruded the folded and metamorphosed IOG rocks. From 3000 to 2500 Ma cratonization of the East Indian Shield formed the batholitic mass of Singhbhum granitic complex at the central part with the greenstone belts on either side. Around 2500 Ma the Singhbhum craton became tectonically active again with the formation of three mobile belts – Dalma in the north, Dhanjori-Simlipal in the east and Jagannathpur-Malangtoli in the west.The sediments and lavas of these mobile belts are the major resources of Proterozoic Fe, Ti, Au, U, P, Cu, Pb, Mo, W and Ni mineralization
Keywords
Archean, Metallogeny, Tectonics, East Indian Shield
To cite this article
Tapan Kumar Baidya, Archean Metallogeny and Crustal Evolution in the East Indian Shield, Earth Sciences. Special Issue:Archean Metallogeny and Crustal Evolution. Vol. 4, No. 4-1, 2015, pp. 1-14. doi: 10.11648/j.earth.s.2015040401.11
Reference
[1]
Ball, V.,1981: The geology of Manbhum and Singhbhum. Rec. Geol. Surv. India, 18, pt.2.
[2]
Bose, P.N. ,1904: Notes on the geology and mineral resources of Mayurbhanj. Rec. Geol. Surv. India, 31, 167-173
[3]
Jones, H.C.,1934: The iron ore deposits of Bihar and Orissa. Mem. Geol. Surv. India, 63, pt. 2, 167-302.
[4]
Dunn, J.A.,1940: The stratigraphy of south Singhbhum. Mem. Geol. Surv. India, 63, pt. 3, 303-369.
[5]
Dunn, J.A. and Dey, A.K., 1942: The geology and petrology of eastern Singhbhum and surrounding areas. Mem. Geol. Surv. India, 69, pt. 2, 281-450.
[6]
Sarkar, S.N. and Saha, A.K.,1962: A revision of the Precambrian stratigraphy and tectonics of Singhbhum and adjacent region. Q. J. Geol. Min. Met. Soc. India, 34, 97-136.
[7]
Sarkar, S.N. and Saha, A.K.,1963: On the occurrence of two intersecting Precambrian orogenic belts in Singhbhum and adjacent areas, India. Geol. Mag., 100, 69-92.
[8]
Sarkar, S.N. and Saha, A.K. ,1983: Structure and tectonics of the Singhbhum-Orissa Iron Ore craton, eastern India. In: Rec. Res. Geol., 10, (structure and tectonics of the Precambrian rocks). Hindustan Pub. Corp. India, Delhi, 1-25.
[9]
Saha, A.K.; Ray, S.L. and Sarkar, S.N. ,1988: Early history of the Earth:evidence from the Eastern Indian Shield. Mem.8, Geol.Soc.India, Bangalore, 13-37.
[10]
Saha, A.K. ,1994: Crustal evolution of Singhbhum-North Orissa, Eastern India. Mem.27, Geol.Soc.India, Bangalore, 1-341.
[11]
Sarkar, S.N.; Saha, A.K. and Miller, J.A.,1969: Geochronology of the Precambrian rocks of Singhbhum and adjacent regions, eastern India. Geol. Mag., 106, 15-45.
[12]
Sarkar, S.N.; Saha, A.K. and Miller, J.A.,1977: The present status of the Precambrian stratigraphy, tectonics and geochronology of Singhbhum-Keonjhar-Mayurbhanj region, eastern India. J. Earth Sci., S. Ray Volume, 37-65.
[13]
Banerji, A.K., 1974: On the stratigraphy and tectonic history of the iron ore bearing and associated rocks of Singhbhum and adjoining areas of Bihar and Orissa. J. Geol. Soc. India, 15, 150-157.
[14]
Banerji, A.K., 1977: On the Precambrian banded iron formations and the manganese ores of the Singhbhum region, eastern India. Econ. Geol., 72 (1), 90-98.
[15]
Prasada Rao, G.H.S.V.; Murty, Y.G.K. and Dikshitulu, M.N., 1964: Stratigraphic relation of Precambrian iron formations and associated sedimentary sequences in parts of Keonjhar, Cuttack, Dhenkanal and Sundargarh districts, Orissa, India. Rept. 22nd Inter. Geol. Cong., pt. 10, 72-87.
[16]
Iyenger, S.V.P. and Alwar, M.A., 1965: The Dhanjori eugeosyncline and its bearing on the stratigraphy of Singhbhum, Keonjhar and Myurbhanj districts. D.N. Wadia Commem. Vol., Min. Geol. Met. Inst. India, 138-162
[17]
Mukhopadhyay, D.,1988: Precambrian of the Eastern Indian Shield – perspective of the problem. Mem. Geol. Soc. India, 8, 1-12.
[18]
Chakraborty, K.L. and Majumder, T.,1986: Geological aspects of the Banded Iron Formation of Bihar and Orissa. J. Geol. Soc. India, v.28, 109-133.
[19]
Saha, A.K.; Ray,S.L.; Ghosh, S.; Mukhopadhyay, K. and Dasgupta, D. ,1984: Studies in crustal evolution of the Singhbhum-Orissa Iron ore craton. Monograph on “ Crustal evolution of parts of Indian Shield “. Ind.Soc.Earth Sci., 1-74.
[20]
Shaw, D.M.,1954: Trace elements in pelitic rocks; part-I and –II, Bull. Geol. Soc. Amer., 65, 1151-1182.
[21]
Shaw, D.M.,1956: Geochemistry of pelitic rocks. Part-III, Bull. Geol. Soc. Amer., 67, 919-934.
[22]
Barker, F. and Arth, J.G.,1976: Generation of trondhjemitic-tonalitic liquids and Archean bimodal trondhjemite-basalt suites. Geology, 4, 596-600
[23]
Condie, K.C. and Hunter, D.R.,1976: Trace element geochemistry of Archean granitic rocks from Barberton region, South Africa. Earth Planet. Sci. Lett. 29, 389-400
[24]
Misra, S.; Deomurari, M.P.; Wiedenbeck, M.; Goswami, J.N.; Ray, S. and Saha, A.K.,1999 : 207Pb/206Pb zircon ages and the evolution of the Singhbhum craton, eastern India. an ion microprobe study. Precamb. Res., 93, 139-151.
[25]
Basu, A.R.; Ray, S.L.; Saha, A.K. and Sarkar, S.N.,1981: Eastern Indian 3800 million year old crust and early mantle differentiation. Science, 212, 1502-1506
[26]
Moorbath, S.; Taylor, P.N. and Jones, N.W., 1986: Dating the oldest terrestrial rocks – facts and fiction. Chem. Geology, 57, 63-86
[27]
Moorbath, S. and Taylor, P.N., 1988: Early Precambrian crustal evolution in eastern India: the age of the Singhbhum Granite and included remnants of older gneiss. J. Geol. Soc. India, 31(1), 82-84.
[28]
Saha, A.K.,1972: Petrogenetic and structural evolution of the Singhbhum granite complex, eastern India. Rept. 24th Int. Geol. Cong. Sec. 2, 149-167.
[29]
Saha, A.K.; Sankaran, A.V. and Bhattacharyya, T.K. ,1968: The behavior of trace elements in the magmatic members of Singhbhum granite. J.Geol.Soc.India, 9, 178-196.
[30]
Paul, D.K.; Mukhopadhyay, D.; Pyne T.K. and Bishoi, P.K.,1991: Rb-Sr age of granitoid in the Deo river section, Singhbhum and its relevance to the age of Iron Formation, Ind. Mineral, 45, 51-56.
[31]
Chakraborty, K.L. and Majumder, T., 2002: Some important aspects of the banded iron formation (BIF) of Eastern Indian Shield (Jharkhand and Orissa). Ind. J. Geol., 74 (1-4), 37-47.
[32]
Acharya, S., 2002: The Daitari-Tomka basin – its structural and stratigraphic evolution & genesis of associated iron ores. Ind. J. Geol., 74 (1-4), 49-81.
[33]
Fryer, B.J., 1983: Rare earth elements in iron-formation. In “Iron-Formations: Facts and Problems.” Elsevier (Amsterdam), 345-358.
[34]
Mukhopadhyay, J., Beukes, N.J., Armstrong, R.A., Zimmermann, U, Ghosh, G. and Medda, R.A., 2008: Dating the oldest greenstone belt in India: A 3.51 Ga precise U-Pb SHRIMP zircon age for dacitic lava of the southern Iron Ore Group, Singhbhum craton. J.Geol., 116, 449-461.
[35]
Ghose, N.C., 1983: Geology, tectonics and evolution of the Chhotanagpur granite-gneiss complex, Eastern India. In “Recent Researches in Geology”, Hindustan Pub. (Delhi), 10, 211-247.
[36]
Mahadevan, T.M., 2002: Geology of Bihar & Jharkhand. Geol. Soc. India, Spl. Pub., Ch. 13, 257-314.
[37]
Pandey, B.K., Upadhyay, D.L. and Sinha, K.K., 1986 a: Geochronology of Jajawal-Binda-Nagnaha granitoids in relation to uranium mineralization. Ind. J. Earth Sci., 13 (2-3), 163-168.
[38]
Pandey, B.K., Gupta, J.N. and Lall, Y., 1986 b: Whole rock and mineral isochron ages for the granites from Bihar mica belt of Hazaribagh, Bihar, India. Ind. J. Earth Sci., 13 (2-3), 157-162.
[39]
Dunn, J. A., 1929: The geology of north Singhbhum including parts of Ranchi and Manbhum districts. Mem. Geol. Surv. India, 54, pt. 2.
[40]
Baidya, T.K. and Chakravarty, P.S., 1988: Mineralization in the Belamu-Jaipur sector of northwestern Purulia district, West Bengal. Geol. Soc. India Mem.8, 147-165.
[41]
Saha,A.K., Bose,R.,Ghosh, S.N. and Roy,A.,1977: Petrology and emplacement of the Mayurbhanj Granite batholiths, eastern India. Bull.Geol.Min.Met.Soc.India,49(Pt-2), 1-34 .
[42]
Iyenger, S.V.P., Chandy, K.C. and Narayanswamy, R, 1981: Geochronology and Rb-Sr systematic of the igneous rocks of the Simlipal Complex, Orissa. Ind. J. Earth Sci., 8, 61-65
[43]
Sengupta, S., Paul, D.K., De Laeter, J.R., Menaughton, N.J., Bandyopadhyay, P.K. and De Smeth, J.B., 1991: Mid-Archean evolution of the Eastern Indian craton: Geochemical and isotopic evidence from the Bonai pluton. Precamb. Res., 49, 23-37.
[44]
Bandyopadhyay, P.K., 1981: Chakradharpur granite-gneiss – a composite batholith in the western part of the Singhbhum shear zone, Bihar. Ind. J. Earth Sci., 8, 109-118.
[45]
Bandyopadhyay, P.K., 1983: Some geochemical characteristics of the Chakradharpur granite gneiss body in west Singhbhum and their bearing on its evolution. Q. J. Geol. Min. Met. Soc. India, 65, 137-147.
[46]
Bhaumik, N. and Basu, A., 1984: Tectonic and stratigraphic status of Chakradharpur granite gneiss, Singhbhum. Ind. J. Earth Sci., CEISM Seminar volume, 29-40.
[47]
Ghosh, S.K., 1963: Structural, metamorphic and migmatitic history of the area around Kuilipal, eastern India. Q.J. Geol. Min. Met. Soc. India, 35, 211-234.
[48]
Iyenger, S.V.P. and Banerjee, S., 1964: Magmatic phases associated with the Precambrian tectonics of Mayurbhanj district, Orissa, India. Rept. 22nd Int. Geol. Cong., 10, 515-538.
[49]
Banerjee, P.K., 1982: Stratigraphy, petrology and geochemistryof some Precambrian basic volcanic and associated rocks of Singhbhum district, Bihar and Mayurbhanj and Keonjhar districts, Orissa. Mem. Geol. Surv. India, 111, 54 p.
[50]
Shaw, R.K., Arima, M., Kagami, H., Fanning, C.M., Shriaishi, K. and Motoyoshi, Y., 1997: Proterozoic events in the Eastern Ghats Granulite Belt, India: Evidence from Rb-Sr, Sm-Nd sytematics and SHRIMP dating. Jour. Geol., 105, 645-656.
[51]
Spencer, E. and Percival, F.G., 1952: The structure and origin of the banded hematite jasper of Singhbhum, India. Econ. Geol., 67, 365-385.
[52]
Dunn, J. A., 1937: The mineral deposits of eastern Singhbhum and surrounding areas. Mem. Geol. Surv. India, 69, pt. 1.
[53]
Dunn, J. A., 1935: The origin of iron ores in Singhbhum, India. Econ. Geol., 30, 643-654
[54]
Beukes, N.J., Mukhopadhyay, J. and Gutzmer, J., 2008: Genesis of high-grade iron ores of the Archean Iron Ore Group around Noamundi, India. Econ. Geol., 103, 365-386.
[55]
Klein, C. and Beukes, N.J., 1992: Time distribution, stratigraphy and sedimentologic setting, and geochemistry of Precambrian iron formations, in Schopf. J.W. and Klein, C. eds., The Proterozoic biosphere: Cambridge University Press, 139-146.
[56]
Roy, S., 1968: Mineralogy of different genetic types of manganese deposits. Econ. Geol., 63, 760-788.
[57]
Murthy, V.N. and Ghosh, B.K., 1971: Manganese ore deposits of Bonai-Keojhar belt, Orissa. Ind. Minerals, 25, 201-210.
[58]
Majumder, T., Chakraborty, K.L. and Bhattacharyya, A., 1982: Geochemistry of Banded Iron Formation of Orissa, India. Mineralium Deposita, 17, 107-118.
[59]
Majumder, T., Whitley, J.E. and Chakraborty, K.L., 1984: Rare earth elements in the Indian Banded iron formation. Chem. Geol., 45, 203-211.
[60]
Banerjee, S., 1960: Genesis of the chromite ores of Jojohatu, Singhbhum dist., Bihar, India with a note on their mineralogy. Proc. Nat. Inst. Sci. India, 26A (1), 31-40.
[61]
Singh, K.K., 1964: A chemical study of the chromite ores of Jojohatu, Singhbhum, Bihar. Bull. Dept. of Geol. & Geophys., University of Roorkee, No.1, 29-50.
[62]
Mukherjee, S., 2002: Chromite deposits in Jojohatu area, Singhbhum district, Jharkhand, India – with special reference to ore petrography and ore genesis. M.Sc. thesis, Jadavpur University, Kolkata, 35 p.
[63]
Baidya, T.K., 1975: Geology of the chromite deposits and the associated rocks in and around Kathapal, Dhenkanal district, Orissa, India. M.Sc Thesis, Jadavpur University, Kolkata, 100 p.
[64]
Chakraborty, K.L. and Baidya, T.K., 1978: Geological setting and mineralogy of the chromite and some associated minerals of Kathapal, Dhenkanal district, Orissa. J. Geol. Soc. India, 19 (7), 303-309.
[65]
Banerjee, P.K., 1972: Geology and geochemistry of the Sukinda ultramafic field, Cuttack district, Orissa. Mem. Geol. Surv. India, 103.
[66]
.Basu, A., Maitra, M. and Roy, P.K., 1997: Petrology of mafic-ultramfic complex of Sukinda valley, Orissa. Ind. Minerals, 50, 271-290.
[67]
Chakraborty, K.L and Chakraborty, T.L., 1984: Geological features and origin of the chromite deposits of Sukinda valley, Orissa, India. Min. Deposita., 19, 256-265.
[68]
Mondal, S.K., Ripley, E.M., Li Chusi and Frei, R., 2006: The genesis of Archean chromitites from the Nuasahi and Sukinda massifs in the Singhbhum Craton, India. Precamb. Res. 148, 45-66.
[69]
Baidya, T.K., Mondal, S.K., Balaram, V., Parthasarathy, R., Verma, R. and Mathur, P.K., 1999: PGE-Ag-Au mineralization in a Cu-Fe-Ni sulphide-rich breccia zone of the Precambrian Nuasahi Ultramafic-Mafic Complex, Orissa, India. J. Geol. Soc. India, 54, 473-482.
[70]
Mondal, S.K., Frei, R. and Ripley, E.M., 2007: Os isotope systematic of mesoArchean chromitite – PGE deposits in the Singhbhum Craton (India): Implications for the evolution of lithospheric mantle. Chem. Geol., 244, 391-408.
[71]
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. Precamb.Res., 121, 85-101.
[72]
Baidya, T.K., 2013: Processing of vanadium-bearing titaniferous magnetite ores of eastern India. Final Project Report (Geological Part), Ministry of Steel, Govt. of India, 51 p.
[73]
Roy, S.,1955: Ore microscopic studies of the vanadium-bearing titaniferous iron ores of Mayurbhanj with a detailed note on their texture. Proc.Nat.Instt.Sci.India, XX(6), 691-702.
[74]
Dasgupta, H.C.,1969: Fe-Ni-V oxide ores associated with gabbro rocks around Dublabera, Bihar. Q.J.Geol.Min.Met.Soc.India, 41, 51-64.
[75]
Banerjee, P.K.,1984: On some geochemical features of the vanadiferous magnetite deposits of Kumhardubi and Betjharan, Mayurbhanj district, Orissa. Chem.Geol.,43, 257-269.
[76]
Baidya, T.K., 1996: Prospect for gold in some areas of the Eastern Indian Shield. Proc. Nat. Workshop on ‘Exploaration and Exploitation of Gold resources of India.’ N.G.R.I (Hyderabad), 165-169.
[77]
Sahoo, R.K., Nayak, B.K., Das, S.K. and Chattopadhyay, P., 1996: Gold mineralization in Orissa. Proc. Nat. Workshop on ‘Exploration and Exploitation of Gold resources of India’, N.G.R.I. (Hyderabad), 210-213.
[78]
Page, N.J., Banerji, P.K. and Haffty, J., 1985: Characterization of the Sukinda and Nuasahi ultramafic complexes, Orissa, India by platinum-group element geochemistry. Precamb. Res., 30, 27-41.
[79]
Nanda,J.K., Patra, R.N. and Mishra,R.N.,1996: Petrogenetic history of the platiferous magmatic breccias zone in Baula Igneous Complex: a conceptual model for PGM localization. In “Geology and exploration of Platinum Group, Rare metal and Rare earth elements”.Proc.G.S.I. Workshop, Calcutta, 17-19.
[80]
Das, N.R., Lahiri, S., Basu, D. and Baidya, T.K., 1994: Nuclear techniques to study the noble metals in the chromite-sulphide association of Nuasahi, Orissa, India. Nuclear Geophysics (Pergamon Press, Oxford), 8, 85-90.
[81]
Mondal, S.K. and Baidya, T.K., 1997: Platinum group minerals from the Nuasahi ultramafic – mafic complex, Orissa, India. Min. Mag. (London), 61, 902-906.
[82]
Mondal, S.K., Baidya, T.K., Gururaja Rao, K.N. and Glasscock, M.D., 2001: PGE and Ag mineralization in a breccia zone of the Precambrian Nuasahi ultramafic – mafic complex, Orissa, India. Can. Mineral., 39, 979-996.
[83]
Auge, T., Salpeteur, I., Bailly, L., Mukherjee, M.M., Patra, R.N., 2002: Magmatic and hydrothermal platinum-group minerals and base-metal sulphides in the Baula Complex, India. Can. Mineral., 40, 277-309.
[84]
Mondal, S.K., 2009: Chromite and PGE deposits of MesoArchean ultramafic – mafic suites within the greenstone belts of the Singhbhum Craton, India: Implications for mantle heterogeneity and tectonic setting. J. Geol. Soc. India, 73, 36-51.
[85]
Mondal, S.K., 2011: Platinum Group Element (PGE) geochemistry to understand the chemical evolution of the earth’s mantle. J. Geol. Soc. India, 77, 295-302.
[86]
Auge, T., Salpeteur, I., Mukherjee, M.M. and Patra, R.N., 1999: Platinum-group element mineralizationin the breccia zone of the Baula Nuasahi Complex, Orissa, India. In Mineral Deposits: Processes to processing, Balkema (eds Stanley et.al.),. Proc. 5th Biennial SGA Meeting, London, 701-704.
[87]
Das, S.K., Rajeev, Acharya, B.S., Muralidhar, J. and Sahoo, R.K., 2002: Characterisation of bulk nickeliferous laterites of Sukinda, Orissa. Ind. J. Geol., 74 (1-4), 249-260.
[88]
Sahoo, R.K., Kaaden, G.V.Dand Muller, G., 1979: The mineralogy and geochemistry of nickeliferous laterites of Sukinda, Orissa, India. In: Inter. Seminar on ‘Lateritisation Processes’, Trivandrum, 77-85.
[89]
Ziauddin, M., Kar, P., Dutta, N.R., Ghosh, D.B., Roy, S., Mishra, K.C., Chakraborty, D.C., Murty, K.K. and Mullick, B.B., 1979: Nickel mineralization in the Sukinda ultramafic field, Cuttack Dist.Orissa. Bull. Geol. Surv. India, Sec. A, 43, 517 pp.
[90]
Baidya, T. K., 1989: Archean Plate Tectonics and formation of the Iron Ore basins in the Eastern Indian Shield. Proc. Symposium on “Structure and Dynamics of the Indian lithosphere”, N.G.R.I, Hyderabad, 16-18.
[91]
Ghosh, R., Chakraborty, D., Halder, M., Baidya, T.K., 2015: Minganese mineralization in Archean greenstone belt, Joda-Noamundi sector, Noamundi basin, East Indian Shield. Ore Geology Reviews, 70, 96-109.
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