Česká geologická služba
Virtual museum
Home  > Minerals > Rocks > Plutonites

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. 6370

No. of sample: g6370
Rock: granit (žula), magmatity hlubinné
Description: jeden kus
Localization: Ostrůvek
Author: leg.Tomas 1966
Comment: rozvadovský masív, středně zrnitá biotit- muskovitická albitická žula, Ostrůvek, balvany při silnici z. osady (db.125), list 1 : 50000, St. Knížecí Huť

back

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