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Swiss Journal of Geosciences
Fig. 9 | Swiss Journal of Geosciences

Fig. 9

From: P–T conditions of metabasites within regional metapelites in far-eastern Nepal Himalaya and its tectonic meaning

Fig. 9

P–T diagram of the mafic granulite H2608, showing results from the garnet–clinopyroxene (GC) geothermometer (E&G79: Ellis and Green 1979; P85: Powell 1985) and the garnet–clinopyroxene–plagioclase–quartz (GCPQ) geobarometer (P&H88: Powell and Holland 1988). The GCPQ geobarometer from the P&H88 is calculated using the garnet solution models of Hodges and Spear (1982: H&S82) and Ganguly and Saxena (1984: G&S84)

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