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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. 7784

No. of sample: g7784
Rock: pyroxenit, magmatity hlubinné
Description: jeden kus /vrtné jádro/
Localization: Otov /Nový kramolín/, Dublovická hora, vrt GP z osad
Author: leg. Vejnar, 1945
Comment: Domažlické krystalinikum - poběžovický komplex,

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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]