VESUVIANITE – POTENTIAL INDICATOR MINERAL OF MINERALIZED SKARNS?

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F16%3A00088194" target="_blank" >RIV/00216224:14310/16:00088194 - isvavai.cz</a>
Result on the web
<a href="http://www.jachymov2016.cz/abstracts" target="_blank" >http://www.jachymov2016.cz/abstracts</a>
DOI - Digital Object Identifier
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Result language
angličtina
Original language name
VESUVIANITE – POTENTIAL INDICATOR MINERAL OF MINERALIZED SKARNS?
Original language description
Vesuvianite is a typical mineral for contact metamorphic and metasomatic rocks – skarns, rodingites, skarnoids. Its composition depends on several factors – bulk composition of the intrusive rock and its metasedimentary host, composi-tion of reacting fluids, and PT-conditions. Vesuvianite structure is complex and accommodates a large number of various elements – its general formula is X19Y13Z18T0-5O68W10, where X = Ca, Na, Ln3+, Pb2+, Sb3+; Y = Al, Mg, Fe3+, Fe2+, Ti4+, Mn, Cu, Zn, As3+; Z = Si; T = B; and W = OH, F, Cl, O [1,2,3]. We studied chemical (major, minor and trace elements) com-position of vesuvianite from skarns at 5 selected localities from the Bohemian Massif. VESUVIANITE COMPOSITION The studied samples are compositionally heterogeneous with variable Fe/Mg ratio, Al/R2+ ratio, and variable contents of Ti, Na and F within each locality; core-to-rim zoning was locally observed (increase of Fe, Be, B, Zn, and Sn, decrease of Al, Mg, and F).
Czech name
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Czech description
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Project
<a href="/en/project/GA14-13347S" target="_blank" >GA14-13347S: Variability of light elements (Li, Be, B) in selected rock-forming and accessory minerals from felsic magmatic and metamorphic rocks</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2016
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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