Article ID Journal Published Year Pages File Type
6443704 Gondwana Research 2013 17 Pages PDF
Abstract
► 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.
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Physical Sciences and Engineering Earth and Planetary Sciences Geology
Preview
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
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