Tectonometamorphic evolution of the Svratka Crystalline Complex (NE Bohemian Massif): Evidence for wrench-dominated transpression along the NE margin of the Variscan orogene root

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Authors	ZAVŘELOVÁ Alice MELICHAR Rostislav SOEJONO Igor VERNER Kryštof TAJČMANOVÁ Lucie
Year of publication	2006
Type	Conference abstract
MU Faculty or unit	Faculty of Science
Citation
Description	Structural development of metagranites from considerred unit shows diferrent and anomalous deformation of feldspars vs. quartz. This feature is explained by polygonal recrystalization of feldspars and sliding along grain boundaries.
Related projects:	Interactions among the chemicals, environment and biological systems and their consequences on the global, regional and local scales (INCHEMBIOL)