%0 Journal Article
%T Emplacement, structural and P-T evolution of the  346 Ma Mi et¨ªn Pluton (eastern Tepl¨¢-Barrandian Zone, Bohemian Massif): implications for regional transpressional tectonics
%A Vondrovic L
%A Verner K
%A Buri¨¢nek D
%A Halodov¨¢ P
%J Journal of Geosciences
%D 2012
%I 
%R 10.3190/jgeosci.109
%X The calc-alkaline Mi et¨ªn Pluton (newly dated at 346 Ma ¡À 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 Poli ka Unit (eastern Tepl¨¢-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 ¡ãC and 0.29-0.43 GPa roughly correspond to peak metamorphic evolution of the host volcano-sedimentary rocks of the northwestern part of the Poli ka and Hlinsko units. The Mi et¨ªn Pluton was emplaced into a NNE-SSW oriented transpressional domain, well recognized on a regional scale along the eastern margin of the Tepl¨¢-Barrandian Zone. During, or shortly after, the magma emplacement, the Mi et¨ªn Pluton was affected 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 Poli ka Unit at the bottom and the overlying Hlinsko Unit after 335 Ma.
%K European Variscides
%K Bohemian Massif
%K Mi et¨ªn Pluton
%K emplacement
%K transpression
%K U-Pb zircon dating
%U http://www.jgeosci.org/content/jgeosci.109_vondrovic.pdf