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      The plutonic magmatites (plutonites) resulted from the solidification and crystallization of magma in major depth below the surface. During this process progressive crystallization of silicate melt takes place. This fractionated crystallization cased a magma differentiation and formation of a suite of plutonites. Also assimilation of materials from surrounding rocks of the magmatic chamber affects the composition of plutonites.

žula - pegmatitická žíla v rul g1441	granodiorit amfibolicko-biotitický g1442	greisen s cínovcem g4860	granodiorit g7710	gabrodiorit pyroxen-amfibolický g7929
žula g10613

In the Virtual Museum there are total 369 samples