Structural position of high-pressure felsic to intermediate granulites from NE Moldanubian domain (Bohemian Massif)

Abstract

This work describes metamorphic and structural evolution of Variscan orogenic root rocks. It provides complete picture about exhumation of rocks from the lower crustal level during the early Carboniferous.

Keywords

• granulite
• lower crust
• Bohemian Massif