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Sivaprakash, C. (1984) Petrology of Sillimanite Gneisses from Garividi, Andhra Pradesh. Journal of the Geological Society of India, 25 (11). 735-743

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Reference TypeJournal (article/letter/editorial)
TitlePetrology of Sillimanite Gneisses from Garividi, Andhra Pradesh
JournalJournal of the Geological Society of India
AuthorsSivaprakash, C.Author
Year1984 (November)Volume25
Page(s)735-743Issue11
PublisherGeological Society of IndiaPlaceBangaluru, India
Classification
Not set
LoC
Not set
Mindat Ref. ID17715308Long-form Identifiermindat:1:5:17715308:4
GUID0
Full ReferenceSivaprakash, C. (1984) Petrology of Sillimanite Gneisses from Garividi, Andhra Pradesh. Journal of the Geological Society of India, 25 (11). 735-743
Plain TextSivaprakash, C. (1984) Petrology of Sillimanite Gneisses from Garividi, Andhra Pradesh. Journal of the Geological Society of India, 25 (11). 735-743
In(1984, November) Journal of the Geological Society of India Vol. 25 (11). Geological Society of India
Abstract/NotesSillimanite+K feldspar+quartz±garnet±Fe-Ti oxide-beartng rocks occur associated wIth calc-silicate locks and manganese formations near Ganvidi in Vijayanagaram district of Andhra Pradesh The whole-rock chemistry shows varying rock oxidation ratios which are reflected in the mineralogical assemblages Almandine garnet is oxidized to mixtures of hematite, quartz and hydrous alummosilicates in oxidized rocks and is absent in highly oxidized rocks in the latter, ilmenite is oxidized to mixtures of rutile and hematite Such relatively high temperature alteration/oxidation effects could have occurred with the influx of water Garnet compositions, and the presence of sillimanite + K-feldspar associiation rather than muscovite+quartz, suggest minimum pressures of 6 Kb, temperatures around 700° and XH2O around 0 6 during metamorphism.

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LocalityCitation Details
Garividi deposit, Vizianagaram District, Andhra Pradesh, India

Mineral Occurrences

LocalityMineral(s)
Garividi deposit, Vizianagaram District, Andhra Pradesh, India Rutile, Sillimanite


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