Podrobnosti záznamu

Název
    Emplacement, structural and P-T evolution of the ~346 Ma Miřetín Pluton (eastern Teplá-Barrandian Zone, Bohemian Massif): implications for regional transpressional tectonics
Autor
    Buriánek, David
    Halodová, Patricie
    Kachlík, Václav
    Míková, Jitka
    Verner, Kryštof
    Vondrovic, Lukáš
Jazyk
    anglicky
Typ dokumentu
    článek v periodiku
Zdrojový dokument - seriál
    Journal of Geosciences
Svazek/č.
    Roč. 56, č. 4
Strany
    15
Rok
    2011
Výraz tezauru
    European Variscides, Bohemian Massif, Miřetín Pluton, emplacement, transpression, U-Pb zircon dating
Klíčové slovo
    346
    Bohemian
    Eastern
    Emplacement
    Evolution
    Implications
    Massif
    Miřetín
    P-T
    Pluton
    Regional
    Structural
    Tectonics
    Teplá-Barrandian
    Transpressional
    Zone
Abstrakt (anglicky)
   The calc-alkaline Miřetín Pluton (newly dated at 346 Ma ? 5 Ma; an U-Pb age obtained by laser-ablation ICP MS method on zircons) is a NNE-SSW elongated intrusive body emplaced into the upper- to mid- crustal rocks of the Polička Unit (eastern Teplá-Barrandian Zone; Bohemian Massif). Its composition reveals similarities to other calc-alkaline granitoids, which are mostly interpreted as products of magma mixing between the basic magmas derived from mantle wedge above a subduction zone with crustally-derived acid melts. The conditions of magma crystallization estimated at 653-681 °C and 0.29-0.43 GPa roughly correspond to peak metamorphic evolution of the host volcano-sedimentary rocks of the northwestern part of the Polička and Hlinsko units. The Miřetín Pluton was emplaced into a NNE-SSW oriented transpressional domain, well recognized on a regional scale along the eastern margin of the Teplá-Barrandian Zone. During, or shortly after the magma emplacement, the Miřetín Pluton was affecte
   d by pervasive submagmatic to high-T solid-state deformation, reflecting an additional strain increment of regional transpression in a narrow zone of thermal softening. Sharply superimposed low-T solid-state fabric preserved along the western part of the Pluton was connected with normal shearing between the Polička Unit at the bottom and the overlying Hlinsko Unit after 335 Ma.
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (RIV)
Zdrojový formát
    R
Datum importu
    15. 10. 2014