Forearc deformation and strain partitioning during growth of a continental magmatic arc: The northwestern margin of the Central Bohemian Plutonic Complex, Bohemian Massif

Abstract

The paper describes deformation of the Tepla-Barrandian unit of the Bohemian Massif during the Variscan orogeny in the area of the northwestern margin of the Central Bohemian Plutonic Complex in the central part of the Bohemian Massif

Keywords

• Anisotropy of magnetic susceptibility (AMS)
• Bohemian Massif
• Central Bohemian Plutonic Complex
• Emplacement
• Magmatic arc
• Teplá–Barrandian unit