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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. 8255

No. of sample: g8255
Rock: granit (žula), magmatity hlubinné
Description: jeden kus
Localization: Branice, o. Písek, lom Bučina, 2100m SZ obce, 180m S k. 540,8, db. 433
Author: leg. Kodym, 1970
Comment: Moldanubikum - česká větev - podolský komplex, výbrus 85710/I, Veselíčko

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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]