Low-pressure granulites of the Lisov Massif, Southern Bohemia: Visean metamorphism of Late Devonian plutonic arc rocks

Abstract

The mafic-intermediate Lisov granulites are thought to have originated during Visean metamorphic overprinting of metaluminous, medium-K calc-alkaline plutonic rocks that formed the mid-crustal root of a Late Devonian magmatic arc

Keywords

• low-pressure granulites
• geothermobarometry
• laser-ablation ICP-MS zircon dating
• whole-rock geochemistry
• Sr-Nd isotopes
• Moldanubian Zone