Synopses: Hornblendes are not common in the charnockites of Kondpalli, but occur as an important constituent in the pyroxene granulites and pyroxenites of Seshadripuram hill. Analyses and optical data for two pargasites are given.
Mineralogical Magazine; June 1978 v. 42; no. 322; p. 280; DOI: 10.1180/minmag.1978.042.322.20
© 1978, The Mineralogical Society
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