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Two-pyroxene mafic granulites from Patharkhang, Shillong-Meghalaya Gneissic Complex

dc.contributor.authorDwivedi S.B.; Theunuo K.
dc.date.accessioned2025-05-24T09:55:43Z
dc.description.abstractThe two-pyroxene mafic granulite of Patharkhang area belongs to the Shillong-Meghalaya Gneissic Complex and includes orthopyroxene-clinopyroxene-hornblende-plagioclase ± quartz as common mineral assemblages, which are stable at thermal peak of regional metamorphism. In this study electron probe microanalysis data have been used to discuss mineral chemistry and pressure-temperature (P-T) condition of metamorphism of the mafic granulite. The average P-T condition suggests a thermal peak of metamorphism at 1029 ± 62°C/7.6 ± 1.7 kbar.
dc.identifier.doiDOI not available
dc.identifier.urihttp://172.23.0.11:4000/handle/123456789/20143
dc.relation.ispartofseriesCurrent Science
dc.titleTwo-pyroxene mafic granulites from Patharkhang, Shillong-Meghalaya Gneissic Complex

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