Chromite and PGE deposits of mesoarchaean ultramafic-mafic suites within the greenstone belts of the Singhbhum craton,India: Implications for mantle heterogeneity and tectonic setting |
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| Authors: | Sisir K Mondal |
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| Institution: | 1.Department of Geological Sciences,Jadavpur University,Kolkata,India;2.Nordic Center for Earth Evolution (NordCEE), Geological Museum,University of Copenhagen,Copenhagen K,Denmark |
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| Abstract: | The Archaean cratonic nuclei of the continents are important as they contain the most significant evidences for the evolution
of Earth e.g. the greenstone sequences. In the Indian Shield, one of the important cratons is the Singhbhum craton, where
nearly 95% of the Indian chromite deposits and only PGE deposits are located which are hosted within Mesoarchaean ultramafic-mafic
rock sequences. The ultramafic units occur as sill like intrusions within the Iron Ore Group (IOG) greenstone belts and often
associated with gabbroic intrusions. In the Nuasahi and Sukinda mining districts of these occurrences, detailed petrological,
geochemical and isotopic studies have been carried out in the last decades. Petrological and geochemical studies indicate
a supra-subduction zone (SSZ) tectonic settings in Archaean for the origin of these ultramafic-mafic sequences. The Os isotopic
and platinum group element (PGE) geochemical studies of chromites from the two mining districts indicate presence of a subchondritic
source mantle domain beneath and within the Singhbhum craton similar to the Zimbabwean craton of southern African continent.
The Os model age calculation indicates melt extraction from a subcontinental lithospheric mantle (SCLM) before 3.7 Ga which
is similar to the other ancient cratons. As a whole the study supports the premise that India was part of the African continent
in pre-Gondwana times and even in early Archaean and suggest possible amalgamation and building up of a supercontinent during
late Archaean. However, in comparison with other occurrences, the Singhbhum craton of the Indian Shield and the Zimbabwean
craton in southern Africa are characterized by the presence of subchondritic lithospheric mantle domains within the SCLM,
which were developed prior to 3.7 Ga. |
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| Keywords: | Chromite PGE Os isotope SCLM Plate tectonics Supercontinent Greenstone belt Archaean Singhbhum craton |
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