Magnetic fabrics in garnet peridotites-pyroxenites and host felsic granulites in the South Bohemian Granulites (Czech Republic): Implications for distinguishing between primary and metamorphism induced fabrics

► Garnet peridotites with layers of garnet pyroxenite occur in HP felsic granulite. ► Magnetic fabric in ultramafite enclaves clearly differs from that in the host granulite. ► Magnetic anisotropy and textural relations show preservation of mantle fabrics in ultramafites.