| Reference Type | Journal (article/letter/editorial) |
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| Title | Feldspars and pryoxenes from the charnockite aeries of Visakhapatnam area, Andhra Pradesh, India |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Murty, M. S. | Author |
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| Year | 1965 (June) | Volume | 35 |
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| Issue | 270 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_35/35-270-393.pdf+ |
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| DOI | doi:10.1180/minmag.1965.035.270.13Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5882 | Long-form Identifier | mindat:1:5:5882:1 |
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| GUID | 0 |
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| Full Reference | Murty, M. S. (1965) Feldspars and pryoxenes from the charnockite aeries of Visakhapatnam area, Andhra Pradesh, India. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 393-400 doi:10.1180/minmag.1965.035.270.13 |
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| Plain Text | Murty, M. S. (1965) Feldspars and pryoxenes from the charnockite aeries of Visakhapatnam area, Andhra Pradesh, India. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 393-400 doi:10.1180/minmag.1965.035.270.13 |
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| In | (1965) Mineralogical Magazine Vol. 35 (270) Mineralogical Society |
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| Abstract/Notes | SummaryA twin-law study of the plagioclase indicated metamorphic origin of the charnockites and volcanic origin of the basic members of the charnockite series. The original volcanic products have been influenced by the later metamorphism, resulting in the various basic members. The twinning in the plagioclase is considered to be primary. The perthite in the charnockite is of orthoclase variety and indicates a higher temperature of formation than the charnockites of other areas containing microcline. The orthopyroxene in the charnockite series is hypersthene and the clinopyroxene is sahlite. Hypersthene is inferred to have formed at the expense of sahlite, hornblende, biotite, and garnet. |
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