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Geological Society, London, Special Publications

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Mineral-fluid interactions in the late Archean Closepet granite batholith, Dharwar craton, southern India

Ewa Slaby, Katarzyna Gros, Hans-Jürgen Förster, Alicja Wudarska, Łukasz Birski, View ORCID ProfileMorihisa Hamada, Jens Götze, Hervé Martin, Mudlappa Jayananda, Jean-François Moyen and Izabela Moszumańska
Geological Society, London, Special Publications, 489, https://doi.org/10.1144/SP489-2019-287
Ewa Slaby
Institute of Geological Sciences PAS, Warsaw 00-818, Poland
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Katarzyna Gros
California Institute of Technology Division of Geological and Planetary Sciences
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Hans-Jürgen Förster
Helmholtz-Zentrum Potsdam Deutsches Geoforschungszentrum Potsdam
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Alicja Wudarska
Institute of Geological Sciences, PAS
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Łukasz Birski
California Institute of Technology Division of Geological and Planetary Sciences
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Morihisa Hamada
Departament of Solid Earth Gechemistry Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
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Jens Götze
Institute of Mineralogy, TU Bergakademie Freiberg
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Hervé Martin
Universite Blaise Pascal
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Mudlappa Jayananda
Centre for Earth, Ocean and Atmospheric Sciences, University of Hyderabad
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Jean-François Moyen
Departament de Geologie, Universite Jean Monnet, Saint-Etienne
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Izabela Moszumańska
Institute of Geological Sciences, PAS
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Abstract

The chemical compositions of different rocks as well as volatile-bearing, and volatile-free minerals have been used to assess the presence of fluids in the Closepet batholith and to estimate the intensity of the fluid-rock interactions. The data were processed using polytopic vector analysis (PVA). Additional data include measurements of water content in the structure of volatile-free minerals and an examination of growth textures. The compositions of mineral domains indicated formation/transformation processes with common fluid-mineral interactions. In general, the results suggested that the processes occurred in a ternary system. Two end-members were likely magmas, and the third was enriched in fluids. In contrast, analysis of the apatite domains indicated that they likely formed/transformed in a more complex, four-component system. This system was fluid-rich and included hybrid magma with a high mafic component. PVA implies that the fluids do not appear to come from one source, given their close affinity and partial association with mantle-derived fluids. A dynamic tectonic setting promoting heat influx and redistribution, and interaction of fluids suggests that the formation/transformation processes of minerals and rocks occurred in a hot-spot like environment.

Supplementary material at https://doi.org/10.6084/m9.figshare.c.4356926

  • © 2019 The Author(s). Published by The Geological Society of London. All rights reserved

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Geological Society, London, Special Publications: 473 (1)
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Mineral-fluid interactions in the late Archean Closepet granite batholith, Dharwar craton, southern India

Ewa Slaby, Katarzyna Gros, Hans-Jürgen Förster, Alicja Wudarska, Łukasz Birski, Morihisa Hamada, Jens Götze, Hervé Martin, Mudlappa Jayananda, Jean-François Moyen and Izabela Moszumańska
Geological Society, London, Special Publications, 489, 8 January 2019, https://doi.org/10.1144/SP489-2019-287
Ewa Slaby
Institute of Geological Sciences PAS, Warsaw 00-818, Poland
  • Find this author on Google Scholar
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  • Search for this author on this site
  • For correspondence: e.slaby@twarda.pan.pl
Katarzyna Gros
California Institute of Technology Division of Geological and Planetary Sciences
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Hans-Jürgen Förster
Helmholtz-Zentrum Potsdam Deutsches Geoforschungszentrum Potsdam
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Alicja Wudarska
Institute of Geological Sciences, PAS
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Łukasz Birski
California Institute of Technology Division of Geological and Planetary Sciences
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Morihisa Hamada
Departament of Solid Earth Gechemistry Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
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  • ORCID record for Morihisa Hamada
Jens Götze
Institute of Mineralogy, TU Bergakademie Freiberg
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Hervé Martin
Universite Blaise Pascal
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Mudlappa Jayananda
Centre for Earth, Ocean and Atmospheric Sciences, University of Hyderabad
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Jean-François Moyen
Departament de Geologie, Universite Jean Monnet, Saint-Etienne
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Izabela Moszumańska
Institute of Geological Sciences, PAS
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Mineral-fluid interactions in the late Archean Closepet granite batholith, Dharwar craton, southern India

Ewa Slaby, Katarzyna Gros, Hans-Jürgen Förster, Alicja Wudarska, Łukasz Birski, Morihisa Hamada, Jens Götze, Hervé Martin, Mudlappa Jayananda, Jean-François Moyen and Izabela Moszumańska
Geological Society, London, Special Publications, 489, https://doi.org/10.1144/SP489-2019-287
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