C.J. Hughes
Abstract
Summary The biotite selvedges around potash-feldspar rich leucosome material in migmatites originate at phase boundaries between rocks containing hydrothermal and silicate pore-fluids and are thus indicative of incipient anatexis.
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Summary The biotite selvedges around potash-feldspar rich leucosome material in migmatites originate at phase boundaries between rocks containing hydrothermal and silicate pore-fluids and are thus indicative of incipient anatexis.
Key concepts: Migmatite, Anatexis, Biotite, Geology, Feldspar, Geochemistry, Mineralogy, Petrology