Abstract
One atmosphere experimental study on fresh basaltic rocks of Paleoarchean western Iron Ore Group (IOG) basin of Singhbhum Craton, Eastern India gives insight of the crystallization behavior of the parent magma, liquid lines of descent and appearance of the different constituent phases. The natural starting material is sufficiently ferroan (FeOt: 14.28 wt%) and corresponds to ‘ferro-basalt’. Regarding the experimental run products, clinopyroxene shows Al2O3 rich character (ranging from 2.23–6.94 wt%; formed due to fluctuating silica activities in the magma) while plagioclase reveals typical Fe-Mg enrichment (that corresponds to higher KdFe-Mg between plagioclase and the parent liquid caused due to immiscible silicate melt inclusion in plagioclase where Mg enters more readily in plagioclase than Fe). The run-product glass corresponds to both high and low iron contents suggesting liquid immiscibility in the parent magma at particular temperature-domains. This study suggests that the crystallization of the western Iron Ore Group basalts represents a broad ‘Skaergaard analogue’ involving depression/shift of eutectic point in the diopside-anorthite system during crystallization.
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References
Acharyya, S.K. (1993) Greenstones from Singhbhum Craton, their Archaean character, oceanic crustal affinity and tectonics. Proc. Nat. Acad. Sci., India Section A, v.63A, pp.211–222.
Banerjee, M., Ray, J., Adhikary, N., Nandy, S., Manikyamba, C., Paul, M., Chakraborty, D. and Eslami, A. (2016) Experimental studies to constrain parental magma of Malangtoli volcanics from Singhbhum Craton of the Eastern Indian Shield. Jour. Geol. Soc. India, v.88, pp.245–255.
Basu, A.R., Bandyopadhyay, P.K., Chakraborti, R. and Zou, H. (2008) Large 3.4 Ga Algoma type BIF in the Eastern Indian Craton. Goldschmidt Conf. Abst. Vol., Geochim. Cosmochim. Acta, 72, A59.
Bowen, N.L. (1915) The later stages of the evolution of the igneous rocks. Jour. Geol., v.23, pp.1–89.
Byerly, G.R. and Lowe, D.R. (2014) Paleoarchean ocean crust and mantle excavated by meteor impact: insight into early crustal processes and tectonics. Geology, v.42, pp.635–638.
Cashman, K.V. (1993) Relationship between plagioclase crystallization and cooling rate in basaltic melts. Contrib. Mineral. Petrol., v.113, pp.126–142.
Charlier, B. and Grove, T.L. (2012) Experiments on liquid immiscibility along tholeiitic liquid lines of descent. Contrib. Mineral. Petrol., v.164(1), pp.27–44.
Deer, W.A., Howie, R.A. and Zussman, J. (1992) An Introduction to the Rock-Forming Minerals (2nd Ed.). Longman Scientific and Technical, Essex, England, 696p.
Fagan, T.J., Taylor, G.J., Keil, K., Hicks, T.L., Killgore, M., Bunch, T.E., Wittke, J.H., Mittlefehldt, D.W., Clayton, R.N., Mayeda, T.K., Eugster, O., Lorengetti, S. and Norman, M.D. (2003) Northwest Africa 773: Lunar origin and iron enrichment trend. Meteorit. Planet. Sci., v.38(4), pp.529–554.
Ghiorso, M.S. and Sack, R.O. (1995) Chemical mass transfer in magmatic processes IV: a revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid solid equilibria in magmatic systems at elevated temperatures and pressures. Contrib. Mineral. Petrol., v.119, pp.197–212.
Irvine, T.N. and Baragar, W.R.A. (1971) A guide to the chemical classification of the common volcanic rocks. Can. Jour. Earth Sci., v.8, pp.523–548.
Juster, T.C., Grove, T.L. and Perfit, M.R. (1989) Experimental constraints on the generation of Fe-Ti basalts, andesites, and rhyodacites at the Galapagos spreading centre, 85°W and 95°W. Jour. Geophys. Res., v.94, pp.9251–9274.
Lundgaard, K.L. and Tegner, C. (2004) Partitioning of ferric and ferrous iron between plagioclase and silicate melt. Contrib. Mineral. Petrol., v.147, pp.470–483.
Morimoto, N. (1989) Nomenclature of pyroxenes. Canandian Mineral., v.27, pp.143–156.
Mukhopadhyay, D. and Matin, A. (2020) The Architecture and Evolution of the Singhbhum Craton. Episodes, v.43, pp.19–50.
Mukhopadhyay, J., Beukes, N.J., Armstrong, R.A., Zimmermann, U., Ghosh, G. and Medda, R.A. (2008) Dating the Oldest Greenstone in India: A 3.51 Ga Precise U-Pb SHRIMP Zircon Age for Dacitic Lava of the Southern Iron Ore Group, Singhbhum Craton. Jour. Geol., v.116(5), pp.449–461.
Namur, O., Charlier, B., Pirard, C., Hermann, J., Liégeois, J.P. and Auwera, J.V. (2011) Anorthosite formation by plagioclase flotation in ferrobasalt and implications for the lunar crust. Geochim. Cosmochim. Acta, v.75, pp.4998–5018.
Philpotts, A.R. (1981) Liquid immiscibility in silicate melt inclusions in plagioclase phenocrysts. Bull. Minéral., v.104, pp.317–324.
Philpotts, A.R. (1982) Compositions of immiscible liquids in volcanic rocks. Contrib. Mineral. Petrol., v.80(3), pp.201–218.
Rahman, S. (1975) Some aluminous clinopyroxenes from Vesuvius and Monte Somma, Italy. Mineral. Mag., v.40, pp.43–52.
Roedder, E. and Weiblen, P.W. (1971) Petrology of silicate melt inclusions, Apollo 11 and 12, and terrestrial equivalents. Proc. 2nd Lunar Sci. Conf., Geochim. Cosmochim. Acta., Suppl. 2, v.1, pp.507–528.
Saha, A.K. (1994) Crustal Evolution of Singhbhum-North Orissa, Eastern India. Mem. Geol. Soc. India, no.27, 341p.
Sarkar, S.C. and Gupta, A. (2012) Crustal Evolution and Metallogeny in India. Cambridge University Press, London, 840p.
Sharma, R.S. (2009) Cratons and Fold belts of India. Springer Verlag, Heidelberg, 324p.
Tegner, C. (1997) Iron in plagioclase as a monitor of the differentiation of the Skaergaard intrusion. Contrib. Mineral. Petrol., v.128, pp.45–51.
Toplis, M.J. and Carroll, M.R. (1995) An Experimental Study of the Influence of Oxygen Fugacity on Fe-Ti Oxide Stability, Phase Relations, and Mineral-Melt Equilibria in Ferro-Basaltic Systems. Jour. Petrol., v.36(5), pp.1137–1170.
Acknowledgements
This work is an outcome of collaborative research project between Department of Geology, University of Calcutta and Central Petrological Laboratory, Geological Survey of India (GSI), Kolkata, India. The authors are thankful to the authority of Geological Survey of India for according necessary permission to publish this paper. Sincere thanks are due to the concerned scientists of GSI for their whole-hearted help and co-operation during XRF and EPMA studies. C. Manikyamba is thankful to the Director, NGRI for encouragement and support. Incisive comments from the anonymous reviewer to upgrade the quality of the paper are thankfully acknowledged. Authors also thank Dr. Sandeep Singh for editorial handling.
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Style of Fractional Crystallization in Basalts from the Paleoarchean Western Iron Ore Group of Singhbhum Craton, Eastern India: Implications from One Atmosphere Experimental Studies
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Mahapatra, R.R., Mukherjee, P., Paul, M. et al. Style of Fractional Crystallization in Basalts from the Paleoarchean Western Iron Ore Group of Singhbhum Craton, Eastern India: Implications from One Atmosphere Experimental Studies. J Geol Soc India 98, 627–634 (2022). https://doi.org/10.1007/s12594-022-2037-7
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DOI: https://doi.org/10.1007/s12594-022-2037-7