Record details

Name
    Powell, Roger
Author of Article
    Can Ternary Feldspars be Used to Constrain the Metamorphic Conditions of High-Grade Meta-Igneous Rocks? Evidence from Orthopyroxene Gneisses, Bohemian Massif
    Can ternary feldspars be used to constrain the metamorphic conditions of high-grade meta-igneous rocks? Evidence from orthopyroxene gneisses, Bohemian Massif
    Constraining the metamorphic conditions of high-grade meta-igneous rocks in the Moldanubian of the Bohemian Massif
    Constraining the P-T path of a MORB-type eclogite using pseudosections and garnet zonning: An example from the Bohemian Massif
    Constraining the P-T path of a MORB-type eclogite using pseudosections, garnet zoning and garnet-clinopyroxene thermometry: an example from the Bohemian Massif
    Contrasting metamorphic histories of lenses of high-pressure rocks and host migmatites with a flat orogenic fabric (Bohemian Massif, Czech Republic): a result of tectonic mixing within horizontal crustal flow?
    Does ternary feldspar constrain the metamorphic conditions of high-grade meta-igneous rocks? Evidence from orthopyroxene granulites, Bohemian Massif
    Garnet-Clinopyroxene Intermediate granulites in the St. Leonhard Massif of the Bohemian Massif: Ultrahigh temperature metamorphism at high pressure?
    Garnet-clinopyroxene intermediate granulites in the St. Leonhard Massif of the Bohemian Massif: ultrahigh temperature metamorphism at high pressure?
    Garnet-clinopyroxene intermediate granulites in the St. Leonhard massif of the Bohemian Massif: ultrahigh temperature metamorphism at high pressure or not?
    Geothermobarometry of high-grade metamorphic rocks: examples from the Moldanubian of the Bohemian Massif
    The role of melt infiltration in the formation of migmatitic orthogneiss
    Separate or shared metamorphic histories of eclogites and surrounding rocks? An example from the Bohemian Massif
    Transformation of mylonitic metagranite to migmatite by open-system interactions during melt flow: an example from the Gföhl Unit (Bohemian Massif)
    Transformation of mylonitic metagranite to migmatite by open-system interactions during melt flow: an example from the Gföhl Unit (Bohemian Massif)
    Transforming mylonitic metagranite by open-system interactions during melt flow
    Transforming mylonitic metagranite by open-system interactions during melt flow
    Transforming mylonitic metagranite to migmatite by open-system interactions during melt flow