Magnetic fabric and rheology of co-mingled magmas in the Nasavrky Plutonic Complex (E Bohenia): implications for intrusive strain regime and emplacement mechanism

Abstract

The fabrics of mafic microgranular enclaves(MNE) and of the host granodiorite of the old granodiorite intrusion of the Nasavrky Plutonic Complex (E Bohemia) were investigated by means of magnetic anisotropy.

Keywords

• magmatic fabric