Hydrothermal gold mineralization at the Hira Buddini gold mine,India: constraints on fluid evolution and fluid sources from boron isotopic compositions of tourmaline |
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Authors: | M -S Krienitz R B Trumbull A Hellmann J Kolb F M Meyer M Wiedenbeck |
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Institution: | 1.GeoForschungsZentrum Potsdam, Telegrafenberg,Potsdam,Germany;2.Institut für Mineralogie und Lagerst?ttenlehre, RWTH Aachen,Aachen,Germany;3.Department of Economic Geology,Geological Survey of Denmark and Greenland,Copenhagen K,Denmark |
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Abstract: | We determined the boron isotope and chemical compositions of tourmaline from the Hira Buddini gold deposit within the Archean
Hutti-Maski greenstone belt in southern India to investigate the evolution of the hydrothermal system and to constrain its
fluid sources. Tourmaline is a minor but widespread constituent in the inner and distal alteration zones of metabasaltic and
metadacite host rocks associated with the hydrothermal gold mineralization. The Hira Buddini tourmaline belongs to the dravite–schorl
series with variations in Al, Fe/(Fe+Mg), Ca, Ti, and Cr contents that can be related to their host lithology. The total range
of δ11B values determined is extreme, from −13.3‰ to +9.0‰, but 95% of the values are between −4 and +9‰. The boron isotope compositions
of metabasalt-hosted tourmaline show a bimodal distribution with peak δ11B values at about −2‰ and +6‰. The wide range and bimodal distribution of boron isotope ratios in tourmaline require an origin
from at least two isotopically distinct fluid sources, which entered the hydrothermal system separately and were subsequently
mixed. The estimated δ11B values of the hydrothermal fluids, based on the peak tourmaline compositions and a mineralization temperature of 550°C,
are around +1 and +10‰. The isotopically lighter of the two fluids is consistent with boron released by metamorphic devolatilization
reactions from the greenstone lithologies, whereas the 11B-rich fluid is attributed to degassing of I-type granitic magmas that intruded the greenstone sequence, providing heat and
fluids to the hydrothermal system.
Electronic supplementary material The online version of this article (doi:) contains supplementary material, which is available to authorized users. |
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Keywords: | Boron isotopes Orogenic gold deposits Dharwar craton India Tourmaline |
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