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Petrogenesis and geochronology of the Arkasani Granophyre and felsic Dalma volcanic rocks: implications for the evolution of the Proterozoic North Singhbhum Mobile Belt, east India

Published online by Cambridge University Press:  29 September 2014

H.N. BHATTACHARYA ,
D.R. NELSON ,
E.R. THERN  and
W. ALTERMANN
H.N. BHATTACHARYA*
Affiliation:
Department of Geology, Presidency University, 86/1 College Street, Kolkata 700 073, India
D.R. NELSON
Affiliation:
Department of Geology, Presidency University, 86/1 College Street, Kolkata 700 073, India
E.R. THERN
Affiliation:
Department of Applied Physics, Curtin University of Technology, GPO Box U1987, Perth 6001, Australia
W. ALTERMANN
Affiliation:
Department of Geology, Kumba-Exxaro Chair in Geodynamics, University of Pretoria, Pretoria, South Africa
*
†Author for correspondence: [email protected]
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Abstract

The North Singhbhum Mobile Belt (NSMB) is a 200 km long, curved Proterozoic fold–thrust belt that skirts the northern margin of the Archean Singhbhum Craton of NE India. The Singhbhum Shear Zone (SSZ) developed between the Dhanjori and Chaibasa formations near the southern margin of the NSMB and represents an important Cu-U-P metallotect. A SHRIMP U–Pb zircon date of 1861±6 Ma, obtained for the syn- to post-kinematic Arkasani Granophyre that has intruded the SSZ, provides a minimum age for the prolonged tectonic activity and mineralization along the SSZ and for the time of closure of the Chaibasa and Dhanjori sub-basins. The Dalma Volcanic Belt, a submarine rift-related bimodal mafic-felsic volcanic suite, forms the spine of the NSMB. A SHRIMP U–Pb zircon igneous crystallization date of 1631±6 Ma was obtained for an unfoliated felsic volcanic rock from the base of the Dalma volcanic sequence. These new findings suggest that the different sub-basins in the NSMB evolved diachronously under contrasting tectonic environments and were juxtaposed during a later orogenic movement.

Keywords

Arkasani GranophyreDalma volcanismNorth Singhbhum Mobile BeltSingbhum Shear Zone
Type
Original Articles
Information
Geological Magazine , Volume 152 , Issue 3 , May 2015 , pp. 492 - 503
Copyright
Copyright © Cambridge University Press 2014 

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References

Banerjee, A. K., Bhattacharya, N. C. & Chattaopadhyay, B. 1978. Arkasani granophyres from the Singhbhum shear zone, Bihar. Journal of the Geological Society of India 19, 350–8.Google Scholar
Barbarin, B. 1990. Granitoids: main petrogenetic classification in relation to origin and tectonic setting. Geological Journal 25, 227–38.Google Scholar
Batchelor, R. A. & Bowden, P. 1985. Petrologic interpretation of granitoid rocks series using multicationic parameters. Chemical Geology 48, 43–55.Google Scholar
Bhattacharya, H. N. & Mahapatra, S. 2008. Evolution of the Proterozoic rift margin sediments–North Singhbhum Mobile Belt, Jharkhand-Orissa, India. Precambrian Research 162, 302–16.Google Scholar
Bonin, B. 2007. A-type granites and related rocks: evolution of a concept, problems and prospects. Lithos 97, 1–29.CrossRefGoogle Scholar
Bose, M. K. and Chakraborti, M. K. 1981. Fossil marinal basin from the Indian Shield: a model for the evolution of Singhbhum Precambrian belt, Eastern India. Geologische Rundschau 70, 504–18.Google Scholar
Bose, M. K., Chakrabarti, M. K. & Saunders, A. D. 1989. Petrochemistry of the lavas from Proterozoic Dalma volcanic belt, Singhbhum, eastern India. Geologische Rundschau 78, 633–48.Google Scholar
Boynton, W. V. 1984. Cosmochemistry of the rare earth elements: meteorite studies. In Rare Earth Element Geochemistry (ed. Henderson, P.), pp. 63–114. Elsevier, Amsterdam.Google Scholar
Chattopadhyay, B. 1990. The main hill Arkasani granophyres pluton in the Precambrians of eastern India–a model of two stage intrusion. Indian Journal of Geology 62, 233–48.Google Scholar
Clarke, D. B. 1992. Granitoid Rocks. London: Chapman and Hall, 283 pp.Google Scholar
Compston, W., Williams, I. S. & Meyer, C. 1984. U–Pb geochronology of zircons from lunar breccia 73217 using a sensitive high mass-resolution ion microprobe. Journal of Geophysical Research 89, B252–B534.CrossRefGoogle Scholar
Cox, K. G., Bell, J. D. & Pankhurst, R. J. 1979. The Interpretation of Igneous Rocks. London: George Allen & Unwin Press, 450 pp.Google Scholar
Dunn, J. A. 1929. The geology of north Singhbhum-Orissa including parts of Ranchi and Manbhum districts. Memoir of the Geological Survey of India 54, 1–166.Google Scholar
Dunn, J. A. and Dey, A. K. 1942. Geology and petrology of Eastern Singhbhum and surrounding areas. Memoir of the Geological survey of India 69 (2), 281–456.Google Scholar
Eby, G. N. 1990. The A-type granitoids: a review of their occurrence and chemical characteristics and speculations on their petrogenesis. Lithos 26, 115–34.Google Scholar
Gupta, A. & Basu, A. 2000. North Singhbhum Proterozoicmobile belt, eastern India: a review. Geological Survey of India, Special Publication no. 55, 195–226.Google Scholar
Gupta, A., Basu, A. & Ghosh, P. K. 1980. The Proterozoic ultramafic and mafic lavas and tuffs of the Dalma greenstone belt, Singhbhum, eastern India. Canadian Journal of Earth Science 17, 210–31.CrossRefGoogle Scholar
Jung, S., Hoernes, S., Masberg, P. & Hoffer, E. 1999. The petrogenesis of some migmatites and granites (Central Damara Orogen, Namibia): evidence for disequilibrium melting, wall-rock contamination and crystal fractionation. Journal of Petrology 40, 1241–69.CrossRefGoogle Scholar
Khanna, P. P., Saini, N. K., Mukherjee, P. K. & Purohit, K. K. 2009. An appraisal of ICP-MS technique for determination of REEs: long term QC assessment of silicate rock analysis. Himalayan Geology 30, 95–9.Google Scholar
Mahato, S., Goon, S., Bhattacharya, A., Misra, B. & Bernhardt, H. J. 2008. Thermal-tectonic evolution of the North Singhbhum Mobile Belt (eastern India): a view from the western part of the belt. Precambrian Research 162, 102–27.Google Scholar
Maniar, P. D. & Piccoli, P. M. 1989. Tectonic discrimination of granitoids. Bulletin of the Geological Society of America 101, 635–43.Google Scholar
Mukhopadhyay, D. 1984. The Singhbhum Shear Zone and its place in the evolution of the Precambrian mobile belt of north Singhbhum. Journal of the Indian Society of Earth Science, CEISM Volume, 205–12.Google Scholar
Nelson, D. R. 2006. CONCH: a versatile Visual Basic program for the interactive processing of ion-microprobe data. Computer and Geoscience 32, 1479–98.Google Scholar
Pal, D. C., Chaudhuri, T., McFarlane, C. H., Mukherjee, A. & Sarangi, A. K. 2011. Mineral chemistry and in situ dating of allanite, and geochemistry of its host rocks in the Bagjata Uranium Mine, Singhbhum Shear Zone, India: Implications for the chemical evolution of REE mineralization and mobilization. Economic Geology 106, 1155–71.Google Scholar
Pearce, J. A., Harris, N. B. W. & Tindale, A. G. 1984. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. Journal of Petrology 25, 956–83.Google Scholar
Rollinson, H. R. 1993. Using Geochemical Data: Evolution, Presentation, Interpretation. Hariow: Addsion Wesley Longman, 352 pp.Google Scholar
Roy, A. B. & Bhattacharya, H. N. 2012. Tectonostratigraphic and geochronologic reappraisal constraining the growth and evolution of Singhbhum Archaean Craton, eastern India. Journal of the Geological Society of India 80, 455–69.CrossRefGoogle Scholar
Roy, A., Sarkar, A., Jeyakumar, S., Aggrawal, S. K. & Ebihara, M. 2002. Sm–Nd age and mantle source characteristics of the Dhanjori volcanic rocks, Eastern India. Geochemical Journal 36, 503–18.Google Scholar
Saha, A. K. 1994. Crustal evolution of Singhbhum-North Orissa, eastern India. Geological Society of India, Memoir no. 27, 341 pp.Google Scholar
Sarkar, A. N. 1982. Precambrian tectonic evolution of eastern India: a model of converging microplates. Tectonophysics 86, 363–97.Google Scholar
Sarkar, S. C. 2000. Crustal evolution and metallogeny in the eastern Indian craton. Geological Survey of India, Special Publication no. 55, 169–94.Google Scholar
Sarkar, S. C. & Gupta, A. 2012. Crustal Evolution and Metallogeny in India. Cambridge: Cambridge University Press, 840 pp.Google Scholar
Sarkar, S. C., Gupta, A. & Basu, A. 1992. North Singhbhum Proterozoic mobile belt, eastern India: its character, evolution and metallogeny. In Metallogeny Related to Tectonics of the Proterozoic Mobile Belts (ed. Sarkar, S.C.), pp. 271–305. New Delhi: Oxford and IBH Publishing Co. Google Scholar
Sarkar, S. N. & Saha, A. K. 1977. The present status of the Precambrian stratigraphy, tectonics and geochronology of Singhbhum-Keonjhar Mayurbhanj region, Eastern India. Indian Journal of Earth Science, S. Ray Volume, 37–65.Google Scholar
Sarkar, S. N. & Saha, A. K. 1983. Structure and tectonics of the Singhbhum-Orissa iron ore craton, eastern India. In Structure and Tectonics of Precambrian rocks in India (ed. SinhaRoy, S.), pp. 1–25. Hindusthan Publishing Corporation, New Delhi, Recent Researches in Geology no. 10.Google Scholar
Sengupta, S., Bandyopadhyay, P. K., Van Den Hul, H. J. & Chattopadhyay, B. 1984. Arkasani Granophyre: Proterozoic intraplate acid magmatic activity in the Singhbhum Craton, Eastern India. Neues Jahrbuch für Mineralogie Abhandlung 148, 328–43.Google Scholar
Sengupta, S. & Ghose, S. K. 1997. The kinematic history of the Singhbhum Shear Zone. Proceedings of the Indian Academy of Science (Earth and Planetary Science) 106, 185–96.Google Scholar
Sun, S. S. & McDonough, W. F. 1989. Chemical and isotopic systematic of ocean basalts: implication for mantle composition and processes. In Magmatism in Ocean Basins (eds Saunders, A. D. & Norry, M.), pp. 313–45. Geological Society of London, Special Publication no. 42.Google Scholar
Williams, I. S., Compston, W., Black, L. P., Ireland, T. R. & Foster, J. J. 1984. Unsupported radiogenic Pb in zircon: a case for anomalously high Pb–Pb, U–Pb and Th–Pb ages. Contributions to Mineralogy and Petrology 88, 322–7.Google Scholar
Winchester, J. A. & Floyd, P. A. 1977. Geochemical discrimination of different magma series and their differentiation products using immobile elements. Chemical Geology 20, 325–43.CrossRefGoogle Scholar