Metamorphites
The metamorphic rocks are derived from pre-existing sedimentary and magmatic rocks by mineralogical, chemical, and structural changes, essentially in the solid state, in response to marked changes in temperature and/or pressure (both hydrostatic and oriented), during deeper burial into deeper parts of the Earth´s crust. During these processes parallel orientation of newly formed minerals generally forms (schistosity). Hydrothermal metamorphism represents a special type, because it is related to the migration of solutions near ore veins. Contact metamorphism results from temperature effect near contact with magmatite bodies.
List of exhibitsrula - biotitická, jeden kus, vrtné jádro g1715rula svorová, biotitická, jeden kus g1717 rula biotitická, jeden kus g1718 rula amfibolicko-biotitická, jeden kus g1719 rula, biotitická, kvarcitická, jeden kus g1720 rula biotitická, jeden kus g1721 rula biotitická, jeden kus, vrtné jádro g1722 amfibolit, jeden kus g1724 svor biotitický, jeden kus g1734 rula svorová biototocká, jeden kus g1735 rula biotitická, jeden kus g1736 rula biotitická, jeden kus g1737 amfibolit, jeden kus g1740 rula - amfibolicko-biotitická, jeden kus g1741 rula dvojslídná, jeden kus g1746 amfibolit celistvý, jeden kus g1750 amfibolit s epidotem, jeden kus g1752 břidlice chloriticko-amfibolitická, jeden kus g1754 rula dvojslídná, jeden kus g1764 fylit krevelový, jeden kus g2521 | ||
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Česky 
Virtual museum of the Czech Geological Survey, www.geology.cz, (C) Czech Geological Survey, 2011, v.0.99 [13.12.2011]