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Origin of orthopyroxene-bearing felsic gneiss from the perspective of ultrahigh-temperature metamorphism: an example from the Chilka Lake migmatite complex, Eastern Ghats Belt, India

Published online by Cambridge University Press:  17 September 2020

Sankar Bose Open the ORCID record for Sankar Bose [Opens in a new window] ,
Kaushik Das ,
Junji Torimoto  and
Daniel Dunkley
Sankar Bose*
Affiliation:
Department of Geology, Presidency University, Kolkata, India700073 Hiroshima Institute of Plate Convergence Regions Research (HiPeR), Hiroshima University, Japan739-8526
Kaushik Das
Affiliation:
Department of Earth and Planetary Systems Science, Hiroshima University, Japan739-8526 Hiroshima Institute of Plate Convergence Regions Research (HiPeR), Hiroshima University, Japan739-8526
Junji Torimoto
Affiliation:
Ore Genesis Research Unit, Project Team for Development of New-generation Research Protocol for Submarine Resources, JAMSTEC, Japan
Daniel Dunkley
Affiliation:
Department of Polar and Marine Research, Institute of Geophysics Polish Academy of Sciences, Księcia Janusza 64, PL-01452Warsaw, Poland
*
*Author for correspondence: Sankar Bose, Email: [email protected]
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Abstract

Orthopyroxene-bearing felsic gneiss occurs as foliation-parallel layers and bands together with aluminous granulite, mafic granulite, and quartzofeldspathic granulite in the Chilka Lake migmatite complex of the Proterozoic Eastern Ghats Belt, India. The rock was classified previously as charnockite which underwent granulite-facies metamorphism. Field and textural features of this rock show evidence of the partial melting of a biotite-bearing greywacke protolith. Orthopyroxene with/without garnet and cordierite were produced with K-feldspar as peritectic phases of incongruent melting of presumed metaluminous sediments. Fluid-inclusion data suggest the presence of high-density CO2-rich fluids during peak metamorphism, which are similar to those found in associated aluminous granulite. Whole-rock major and trace element data show wide variability of the source materials whereas REE distributions show enriched LREE and flat HREE patterns. Zircon grains from representative samples show the presence of inherited cores having spot dates (SHRIMP) in the range c. 1790–3270 Ma. The overgrowth on zircon was formed predominantly during c. 780–730 Ma and sporadically during c. 550–520 Ma. Some neoblastic zircons with c. 780–730 Ma ages are also present. U-rich dark zones surrounding cores appear partially metamictised, but spot ages from this zone vary within c. 1000–900 Ma. The <1000 Ma ages represent metamorphism that mirrors the events in associated aluminous granulite. The sources of metaluminous sediments are speculative as the rock compositions are largely modified under granulite-facies metamorphism and partial melting. Considering the accretionary tectonic setting of the Eastern Ghats Belt during the c. 1000–900 Ma time frame, a greywacke-type protolith for the migmatite complex has been proposed.

Keywords

orthopyroxene-bearing felsic gneissEastern Ghats Beltmigmatitepartial meltinggreywacke
Type
Article
Information
Mineralogical Magazine , Volume 84 , Issue 5 , October 2020 , pp. 712 - 737
Copyright
Copyright © The Author(s), 2020. Published by Cambridge University Press on behalf of The Mineralogical Society of Great Britain and Ireland

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Footnotes

Associate Editor: Thomas Mueller

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