Mineralogie a geneze horninových úlomků s pegmatitovou texturou z eluvia serpentinitu u Nové Vsi u Oslavan

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Title in English Mineralogy and genesis of rock fragments with pegmatite texture from serpentinite eluvium at Nová Ves near Oslavany
Authors

PROKOP Jiří LOSOS Zdeněk ČOPJAKOVÁ Renata KARÁSEK Jaromír

Year of publication 2013
Type Article in Periodical
Magazine / Source Bulletin mineralogicko-petrologického oddělení Národního muzea v Praze
MU Faculty or unit

Faculty of Science

Citation
Field Geology and mineralogy
Keywords tourmaline;plagioclase;prehnite;pegmatite
Description The studied locality belongs to peridotite body in the Gfohl Unit (Moldanubian Zone). These peridotites underwent high degree of serpentinisation and are locally penetrated by pegmatites. Rock fragments with pegmatite texture were found in eluvia of isolated serpentinite body situated at Nová Ves. Three groups of samples (NV1, NV2 and NV3) distinct in their internal structure, mineral assemblages and chemical composition of minerals were distinguished.
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