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Leelanandam, C. (1967) Chemical study of pyroxenes from the charnockitic rocks of Kondapalli (Andhra Pradesh), India, with emphasis, on the distribution of elements in coexisting pyroxenes. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (278) 153-179 doi:10.1180/minmag.1967.036.278.01

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Reference TypeJournal (article/letter/editorial)
TitleChemical study of pyroxenes from the charnockitic rocks of Kondapalli (Andhra Pradesh), India, with emphasis, on the distribution of elements in coexisting pyroxenes
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsLeelanandam, C.Author
Year1967 (June)Volume36
Issue278
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_36/36-278-153.pdf+
DOIdoi:10.1180/minmag.1967.036.278.01Search in ResearchGate
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Mindat Ref. ID6060Long-form Identifiermindat:1:5:6060:2
GUID0
Full ReferenceLeelanandam, C. (1967) Chemical study of pyroxenes from the charnockitic rocks of Kondapalli (Andhra Pradesh), India, with emphasis, on the distribution of elements in coexisting pyroxenes. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (278) 153-179 doi:10.1180/minmag.1967.036.278.01
Plain TextLeelanandam, C. (1967) Chemical study of pyroxenes from the charnockitic rocks of Kondapalli (Andhra Pradesh), India, with emphasis, on the distribution of elements in coexisting pyroxenes. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (278) 153-179 doi:10.1180/minmag.1967.036.278.01
In(1966) Mineralogical Magazine Vol. 36 (278) Mineralogical Society
Abstract/NotesSummaryThe chemical analyses, structural formulae, and trace element data are presented for 18 orthopyroxenes and 9 clinopyroxenes from the charnockitie rocks of Kondapalli, Andhra Pradesh, India. The chemistry of these pyroxenes is discussed and conclusions are drawn. The data are compared with the similar data available for the pyroxenes of the charnockites of the type area near Madras, some 200 miles south of Kondapalli. The element-distributional relationships between the coexisting pyroxenes are discussed and inferences are made regarding the temperature of crystallization of charnockite pyroxenes.


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