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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. 7544

No. of sample: g7544
Rock: granodiorit, magmatity hlubinné
Description: jeden kus
Localization: Herbertov
Author: leg.Suk, 1967
Comment: Centrální pluton, 1:50000, Vyšší Brod, g. weinsberský, zářez u želez. stanice

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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]