Granulite (felsic)

The common metamorphic facies. The boundaries between the facies are depicted as wide bands because they are gradational and approximate. P-P = Prehnite-Pumpellyite facies.

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Granulite (felsic)

The rocks with >30% mafic minerals (dominantly pyroxene) may be called mafic granulites, those with <30% mafic minerals (dominantly pyroxene) may be called felsic granulites. Granulite may exhibit a crude gneissic structure due to the parallelism of flat lenses of quartz and/or feldspar. The texture is typically granoblastic.

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GitHub

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Journal of Metamorphic Geology

High-pressure granulites are characterised by the key associations garnet-clinopyroxene-plagioclase-quartz (in basic rocks) and kyanite-K-feldspar (metapelites and felsic rocks) and are typically orthopyroxene-free in both basic and felsic bulk compositions.

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