Record details

    Metamorphic history of skarns, origin of their protolith and implication for genetic interpretation; an example from three units of the Bohemian Massif
    Konopásek, Jiří
    Košler, Jan
    Košuličová, Monika
    Pertold, Zdeněk
    Pertoldová, Jaroslava
    Pudilová, Marta
    Týcová, Patricie
    Verner, Kryštof
Publication type
    článek v periodiku
Source title - serial
    Journal of Geosciences
    Roč. 54, č. 2
Thesaurus term
    skarn, Bohemian Massif, petrology, geochemistry, oxygen isotopes,detrical zircon age
Abstract (in english)
   Skarns in the Svratka Unit, in the neighbouring part of the Moldanubian Zone and in the Kutná Hora Complex were studied with respect to their tectonometamorphic evolution, geochemistry of the major and trace elements, stable isotope geochemistry and zircon ages. The geological positions of skarns, and their structural and metamorphic record probably reflect common tectono-metamorphic evolution with that of the surroundings rocks. The geochemical characteristics, values of the oxygen isotopes and the presence of detrital zircons with a wide range of ages exclude a metasomatic origin of the skarns and point to a sedimentary-exhalative protoliths.
    UK Praha, Přírodovědecká fakulta
Contributor code
    UK, PřF
Source format
Import date
    8. 8. 2012