<style face="normal" font="default" size="100%">High-Ti muscovite as a prograde relict in high pressure granulites with metamorphic Devonian zircon ages (Bestvina granulite body, Bohemian Massif): Consequences for the relamination model of subducted crust</style>

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0<style face="normal" font="default" size="100%">High-Ti muscovite as a prograde relict in high pressure granulites with metamorphic Devonian zircon ages (Bestvina granulite body, Bohemian Massif): Consequences for the relamination model of subducted crust</style><style face="normal" font="default" size="100%">High-Ti muscovite as a prograde relict in high pressure granulites with metamorphic Devonian zircon ages (Bestvina granulite body, Bohemian Massif): Consequences for the relamination model of subducted crust</style>