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Nayak, B. R., Mohapatra, B. K. (1998) Two morphologies of pyrophanite in Mn-rich assemblages, Gangpur Group, India. Mineralogical Magazine, 62 (6) 847-856 doi:10.1180/002646198548070

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Reference TypeJournal (article/letter/editorial)
TitleTwo morphologies of pyrophanite in Mn-rich assemblages, Gangpur Group, India
JournalMineralogical MagazineISSN0026-461X
AuthorsNayak, B. R.Author
Mohapatra, B. K.Author
Year1998 (December)Volume62
Issue6
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_62/62-6-847.pdf+
DOIdoi:10.1180/002646198548070Search in ResearchGate
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Mindat Ref. ID342Long-form Identifiermindat:1:5:342:7
GUID0
Full ReferenceNayak, B. R., Mohapatra, B. K. (1998) Two morphologies of pyrophanite in Mn-rich assemblages, Gangpur Group, India. Mineralogical Magazine, 62 (6) 847-856 doi:10.1180/002646198548070
Plain TextNayak, B. R., Mohapatra, B. K. (1998) Two morphologies of pyrophanite in Mn-rich assemblages, Gangpur Group, India. Mineralogical Magazine, 62 (6) 847-856 doi:10.1180/002646198548070
Abstract/NotesAbstractPyrophanite is widely distributed in metamorphic Mn-rich rock assemblages of the Gangpur Group, India. It occurs in two distinct habits: as an independent phase, and as an exsolved phase within hematite. The well developed large sized crystals coexist with spessartine in Mn-silicate facies rocks. In contrast, the exsolved crystals occur as fine needle/bleb-like crystallites intergrown with hematite in Mn-silicate-oxide facies rocks. Compositionally the exsolved crystals are enriched in iron, present in both the ferric and ferrous states. The two morphologies of pyrophanite attest to their formation under different environmental conditions. The independent pyrophanite is formed from a Mn-Ti rich precursor under low oxygen fugacity conditions while the hematite-pyrophanite intergrowth evolved from an Fe-Mn-Ti rich precursor under higher fO2 conditions.


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