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Dora, M.; Singh, H.; Kundu, A.; Shareef, M.; Randive, K.; Joshi, S. (2014) Tsumoite (BiTe) and associated Ni-PGE mineralization from Gondpipri mafic-ultramafic complex, Bastar Craton, Central India: mineralogy and genetic significance. Open Geosciences, 6 (4). 506-517 doi:10.2478/s13533-012-0185-9

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Reference TypeJournal (article/letter/editorial)
TitleTsumoite (BiTe) and associated Ni-PGE mineralization from Gondpipri mafic-ultramafic complex, Bastar Craton, Central India: mineralogy and genetic significance
JournalOpen Geosciences
AuthorsDora, M.Author
Singh, H.Author
Kundu, A.Author
Shareef, M.Author
Randive, K.Author
Joshi, S.Author
Year2014 (August 17)Volume6
Page(s)506-517Issue4
PublisherWalter de Gruyter GmbH
URL
DOIdoi:10.2478/s13533-012-0185-9Search in ResearchGate
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Mindat Ref. ID9288207Long-form Identifiermindat:1:5:9288207:8
GUID0
Full ReferenceDora, M.; Singh, H.; Kundu, A.; Shareef, M.; Randive, K.; Joshi, S. (2014) Tsumoite (BiTe) and associated Ni-PGE mineralization from Gondpipri mafic-ultramafic complex, Bastar Craton, Central India: mineralogy and genetic significance. Open Geosciences, 6 (4). 506-517 doi:10.2478/s13533-012-0185-9
Plain TextDora, M.; Singh, H.; Kundu, A.; Shareef, M.; Randive, K.; Joshi, S. (2014) Tsumoite (BiTe) and associated Ni-PGE mineralization from Gondpipri mafic-ultramafic complex, Bastar Craton, Central India: mineralogy and genetic significance. Open Geosciences, 6 (4). 506-517 doi:10.2478/s13533-012-0185-9
In(2014, January) Open Geosciences Vol. 6 (4) Walter de Gruyter GmbH
Abstract/NotesAbstract
This paper reports the occurrence of Tsumoite (a bismuth telluride) in the Heti Cu-Ni-PGM prospect, Gondpipri mafic-ultramafic complex, Central India. The Gondpipri complex consists of several tectonically dismembered gabbronorite-gabbro-anorthositic gabbro — olivine gabbro -websterite disposed in ∼10 km long tonalite-trondhjemitegranodiorite (TTG) and charnockite-enderbite suite of rocks. The mineralization occurs in the sulphide zone hosted by gabbro variants. The host rocks have been deformed and metamorphosed to granulite grade and subjected to various degrees of hydrothermal alteration. The mineralization comprises chalcopyrite, pentlandite, pyrrhotite, cubanite, millerite, and pyrite. In addition to these, occur (1) tsumoite (2) PGM in the form of moncheite, merenskyite, Pd-mellonite, and Pt-Pd-Te-Bi-Fe-S alloy.
The present study indicates that the mineralization occurs in two stages related to: (i) magmatic and (ii) hydrothermal remobilization and transport of Cu-rich sulphides, tsumoite and PGM, and their re-deposition in hydrosilicate alteration zones. It is possible that the mineralization at Heti formed at different stages of bismuth activity under variable fS2, T, and fTe2 conditions due to change in total concentration of Te and S and /or cooling. Since the role of S is limited, Te and cooling are important factor influencing mineralogy and composition of tsumoite and associated mineralization. Mineralization occurs in two different modes of occurrences. The early mineralisation occur as blebs, specks and dissemination of sulphides, viz. pyrrhotite, chalcopyrite, pentlandite and minor pyrite ± PGM, whereas later mineralisation occur as stringers, minor veins of sulphides viz. pyrite, millerite, cubanite, sijenite, tsumoite and ± PGM.
Mineral assemblages and textural relationships at Heti has indicated precipitation of tsumoite and associated PGM along fractures and secondary silicates, which confirms their hydrothermal origin.

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LocalityCitation Details
Gondpipri Complex, Maharashtra, India
Heti prospect, Gondpipri Complex, Maharashtra, India

Mineral Occurrences

LocalityMineral(s)
Heti prospect, Gondpipri Complex, Maharashtra, India Augite, Bornite, Chalcopyrite, Chlorite Group, Cubanite, Diopside, Epidote, Fayalite-Forsterite Series, Hypersthene, Ilmenite, Ishkulite, Magnetite, Melonite, Merenskyite, Millerite, Moncheite, Muscovite, Pentlandite, Plagioclase, Pyrite, Pyrrhotite, Sericite, Siegenite, Tsumoite, Violarite


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