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Rao, K. S. R., Rao, A. T., Sriramadas, A. (1969) Porphyritic plagioclase–hornblende–pyroxene granulite from charnockitic rocks of Chipurupalli, Visakhapatnam district, Andhra Pradesh, South India. Mineralogical Magazine, 37 (288) 497-503 doi:10.1180/minmag.1969.037.288.10

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Reference TypeJournal (article/letter/editorial)
TitlePorphyritic plagioclase–hornblende–pyroxene granulite from charnockitic rocks of Chipurupalli, Visakhapatnam district, Andhra Pradesh, South India
JournalMineralogical Magazine
AuthorsRao, K. S. R.Author
Rao, A. T.Author
Sriramadas, A.Author
Year1969 (December)Volume37
Issue288
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_37/37-288-497.pdf+
DOIdoi:10.1180/minmag.1969.037.288.10Search in ResearchGate
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Mindat Ref. ID6323Long-form Identifiermindat:1:5:6323:8
GUID0
Full ReferenceRao, K. S. R., Rao, A. T., Sriramadas, A. (1969) Porphyritic plagioclase–hornblende–pyroxene granulite from charnockitic rocks of Chipurupalli, Visakhapatnam district, Andhra Pradesh, South India. Mineralogical Magazine, 37 (288) 497-503 doi:10.1180/minmag.1969.037.288.10
Plain TextRao, K. S. R., Rao, A. T., Sriramadas, A. (1969) Porphyritic plagioclase–hornblende–pyroxene granulite from charnockitic rocks of Chipurupalli, Visakhapatnam district, Andhra Pradesh, South India. Mineralogical Magazine, 37 (288) 497-503 doi:10.1180/minmag.1969.037.288.10
In(1969, December) Mineralogical Magazine Vol. 37 (288) Mineralogical Society
Abstract/NotesSummaryAn unusual occurrence of porphyritic plagioclase-hornblende-pyroxene granulite (porphyritic basic charnockite) has been observed within the ‘Charnockite region’ of the Eastern Ghats of the Precambrian formations of India. From the X-ray and chemical data the phenocrysts are considered to be augite phenocrysts. Based on petrographic and chemical evidence it is inferred that the basic charnockites of Chipurupalli area in Visakhapatnam district are formed from tholeiitic magma as a gabbroic mass under deep seated plutonic conditions. The gabbroic mass has been recrystallized as plagioclase-hornblende-pyroxene granulite due to later metamorphism, leaving most of the phenocrysts unaffected.


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