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Plutonites

      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.


Exhibition detail no. 6048

No. of sample: g6048
Rock: kvarcdiorit, magmatity hlubinné
Description: jeden kus
Localization: Ořechov - Nebovidy
Author: leg.Dudek 1965
Comment: nehomogenní amfibolicko-biotitický křemenný diorit (granitizovaný amfibolit), list Židlochovice, 1:50000,lom při silnici Ořechov-Nebovidy, 400m s. od mostu přes Bobravu

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Virtual museum of the Czech Geological Survey, www.geology.cz, (C) Czech Geological Survey, 2011, v.0.99 [13.12.2011]