Silicate, oxide and sulphide trends in Neo-Archean rocks from the Nilgiri Block, Southern India: The role of fluids during high-grade metamorphism

Vinod O. Samuel, Daniel E. Harlov, Sanghoon Kwon, K. Sajeev

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4 Citations (Scopus)

Abstract

The Nilgiri Block, southern India represents an exhumed section of lower, late Archean (2500 Ma) crust. The northern highlands of the Nilgiri Block are characterized by metagabbros with pyroxenite inlayers. A two-pyroxene granulite zone acts as a transition between the metagabbros and charnockites, which are exposed in the central and southern part of the Nilgiri highlands. Thermobarometry results indicate a SW-NE regional trend both in temperature (∼650-800°C) and in pressure (700-1100 MPa) over the Nilgiri highlands. In the charnockites, composite rutile-ilmenite grains are the dominant oxide assemblage. In the two-pyroxene granulites, hemo-ilmenite-magnetite is dominant with coexisting rutile-ilmenite composite grains in a few samples in the vicinity of the boundary with the charnockites. In the metagabbros, hemo-ilmenite-magnetite is the dominant oxide assemblage. The principal sulphide mineral in the charnockite is pyrrhotite with minor pyrite-chalcopyrite exsolution lamellae or blebs. In the two-pyroxene granulites and the metagabbros, the principal sulphide assemblage consists of discrete pyrite grains with magnetite rims and pyrite-pyrrhotite-chalcocopyrite associations. From these observations, a specific oxidation trend is seen. The northern granulite-facies metagabbros and two-pyroxene granulites of the Nilgiri highlands are highly oxidized compared with the charnockites from the central and southern regions. This higher oxidation state is proposed to be the result of highly oxidizing agents (probably as SO3) in low H2O activity grain boundary NaCl saline fluids with a dissolved CaSO4 component present during granulite-facies metamorphism of the metagabbros and two-pyroxene granulites. Eventually these agents became more reducing, owing to the inherent buffering of the original tonalite-granodiorite granitoids at the graphite-CO2 buffer, such that S took the form of H2S during the granulite-facies metamorphism of the charnockites. At the same time, these saline fluids were also responsible the solid-state conversion of biotite and amphibole to orthopyroxene and clinopyroxene in the metagabbro, two-pyroxene granulite, and charnockite.

Original languageEnglish
Pages (from-to)1027-1062
Number of pages36
JournalJournal of Petrology
Volume60
Issue number5
DOIs
Publication statusPublished - 2019 May 1

Bibliographical note

Funding Information:
This research was supported by 2017R1A6A1 A07015374 (Multidisciplinary study for assessment of large earthquake potentials in the Korean Peninsula) through the National Research Foundation of Korea (NRF) funded by the Ministry of Science and ICT, Korea to V.O.S, and NRF-2015R1D1A1A09058914 and NRF-2019R1A2C1002211 to S.K. We acknowledge funding from the Ministry of Earth Sciences, Government of India project MoES/ATMOS/PP-IX/09 in developing petrography and sample preparation laboratory facilities at the Centre for Earth Sciences, Indian Institute of Science, Bangalore.

Publisher Copyright:
© 2019 The Author(s). Published by Oxford University Press. All rights reserved.

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology

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