Record details

    Obata, M.
Author of Article
    Kyanite eclogites and high-Mg garnet pyroxenites from the Czech Bohemian Massif were originally formed as cumulative gabbros
    Origin of eclogite and garnet pyroxenite from the Moldanubian Zone of the Bohemian Massif, Czech Republic and its implication to other mafic layers embedded in orogenic peridotites
    Two Contrasting Fabric Patterns of Olivine Observed in Garnet and Spinel Peridotite from a Mantle-derived Ultramafic Mass Enclosed in Felsic Granulite, the Moldanubian Zone, Czech Republic