Magmatic fabrics and emplacement of the cone-sheet-bearing Knížecí Stolec durbachitic pluton (Moldanubian Unit, Bohemian Massif): implications for mid-crustal reworking of granulitic lower crust in the Central European Variscides

Abstract

The ~340 Ma Knížecí Stolec pluton was emplaced as a deep-seated cone-sheet-bearing complex. Prior to emplacement of the magma, the steep sub-concentric foliation in the granulite formed during a buckling event on its exhumation path from greater depths.

Keywords

• durbachite
• emplacement
• exhumation
• granulite
• Moldanubian Unit
• pluton