Mineralogy and genesis of pegmatite-like veins in serpentinite eluvium at Nová Ves near Oslavany (Czech Republic)
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F13%3A00066427" target="_blank" >RIV/00216224:14310/13:00066427 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Mineralogy and genesis of pegmatite-like veins in serpentinite eluvium at Nová Ves near Oslavany (Czech Republic)
Original language description
The features of pegmatite-like vein fragments from Nová Ves are unique in several aspects: (a) extremely variable anorthite content in plagioclases (An02-85); (b) abundance of younger Ca-rich minerals (prehnite, clinozoisite, thompsonite); (c) presence of REE-containing minerals; (d) activity of some volatiles in forming melt (particularly B); (e) only local presence of quartz and K-feldspar and finally; (f) predominant coarse-grained character of primary minerals.
Czech name
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Czech description
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Classification
Type
O - Miscellaneous
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
<a href="/en/project/GAP210%2F10%2F0743" target="_blank" >GAP210/10/0743: Chemical composition and structural order of natural tourmalines - geochemical versus crystal-structural constrains</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2013
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů