Record details

    Magma emplacement during exhumation of the lower- to mid-crustal orogenic root: The Jihlava syenitoid pluton, Moldanubian Unit, Bohemian Massif
Other titles
    Vmístění magmat během exhumace orogenního kořene: Jihlavský syenitový pluton, Moldanubikum, Český masív
    Holub, František
    Hrouda, František
    Verner, Kryštof
    Žák, Jiří
Publication type
    článek v periodiku
Source title - serial
    Journal of Structural Geology
    Roč. 28, č. 8
Thesaurus term
    Anisotropy of magnetic susceptibility (AMS), Emplacement, Exhumation, Pluton, Transtension, Variscan orogeny
Abstract (in czech)
   Vmístění syenitového magmatu během exhumačních procesů
Abstract (in english)
   Structural and AMS data from the 335 Ma ultrapotassic Jihlava syenitoid pluton, which intruded the lower- to mid-crustal orogenic root (Moldanubian Unit) in the Bohemian Massif, Central European Variscides. The emplacement of the pluton was accommodated by multiple processes, such as ductile host-rock shortening, formation of sheeted zones by magma wedging, magmatic stoping, and possibly host-rock displacement within a wide transtensional zone. Magmatic fabrics preserved in the pluton reflect both intrusive processes and regional strain.
    Česká geologická služba
Contributor code
    ČGS (RIV)
Source format
Import date
    15. 10. 2014