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Mineralogie a geneze horninových úlomků s pegmatitovou texturou z eluvia serpentinitu u Nové Vsi u Oslavan
Title in English | Mineralogy and genesis of rock fragments with pegmatite texture from serpentinite eluvium at Nová Ves near Oslavany |
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Authors | |
Year of publication | 2013 |
Type | Article in Periodical |
Magazine / Source | Bulletin mineralogicko-petrologického oddělení Národního muzea v Praze |
MU Faculty or unit | |
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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