. . "Tectonophysics" . "Dragoun, Franti\u0161ek" . . "Kachl\u00EDk, V\u00E1clav" . "Anisotropy of magnetic susceptibility (AMS), Bohemian Massif, Central Bohemian Plutonic Complex, Emplacement, Magmatic arc, Tepl\u00E1\u2013Barrandian unit"@en . . . "6"^^ . "0040-1951" . "[C0D26732676A]" . "NL - Nizozemsko" . . "Forearc deformation and strain partitioning during growth of a continental magmatic arc: The northwestern margin of the Central Bohemian Plutonic Complex, Bohemian Massif"@en . . "Holub, Franti\u0161ek" . "1-4" . "2"^^ . . . . "469" . "The paper describes deformation of the Tepla-Barrandian unit of the Bohemian Massif during the Variscan orogeny. The Late Devonian subduction followed by the Early Carboniferous continental collision of the Saxothuringian and overriding upper-crustal Tepla-Barrandian units led to the growth of a large magmatic arc (the similar to 354-337 Ma Central Bohemian Plutonic Complex) in the central part of the Bohemian Massif. Approaching the magmatic arc margin, the regional structural pattern changes and exhibits significant across- and along-strike variations interpreted as a result of strain partitioning, where the Saxothuringian/Tepla-Barrandian convergence interacted in different ways with the intruding magma pulses." . . . "Forearc deformation and strain partitioning during growth of a continental magmatic arc: The northwestern margin of the Central Bohemian Plutonic Complex, Bohemian Massif"@en . "Verner, Kry\u0161tof" . . "Forearc deformation and strain partitioning during growth of a continental magmatic arc: The northwestern margin of the Central Bohemian Plutonic Complex, Bohemian Massif" . "19"^^ . "P(GP205/07/P226), Z(MSM0021620855), Z(MZP0002579801)" . . "315344" . "Chlup\u00E1\u010Dov\u00E1, Marta" . "RIV/00025798:_____/09:00000206!RIV10-MZP-00025798" . . . "\u017D\u00E1k, Ji\u0159\u00ED" . "RIV/00025798:_____/09:00000206" . "000265990100009" . . . . . "The paper describes deformation of the Tepla-Barrandian unit of the Bohemian Massif during the Variscan orogeny. The Late Devonian subduction followed by the Early Carboniferous continental collision of the Saxothuringian and overriding upper-crustal Tepla-Barrandian units led to the growth of a large magmatic arc (the similar to 354-337 Ma Central Bohemian Plutonic Complex) in the central part of the Bohemian Massif. Approaching the magmatic arc margin, the regional structural pattern changes and exhibits significant across- and along-strike variations interpreted as a result of strain partitioning, where the Saxothuringian/Tepla-Barrandian convergence interacted in different ways with the intruding magma pulses."@en . "Forearc deformation and strain partitioning during growth of a continental magmatic arc: The northwestern margin of the Central Bohemian Plutonic Complex, Bohemian Massif" . . .