Tourmaline from Věžná I pegmatite; an indicator of external contamination and internal fractionation

Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F17%3A00097091" target="_blank" >RIV/00216224:14310/17:00097091 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Jazyk výsledku
angličtina
Název v původním jazyce
Tourmaline from Věžná I pegmatite; an indicator of external contamination and internal fractionation
Popis výsledku v původním jazyce
Minerals of the tourmaline group are chemically very variable and therefore are good indicators of the degree of fractionation and pegmatite contamination. A typical example is the Věžná I locality. There were 6 types of tourmalines found in different zones of pegmatite. In the outer zones, Mg rich dravite predominates, replacing by schorl and foitite, and in the most fractionated parts by Mn and Li rich elbait and fluor-elbait. Tourmalines from more fractionated zones are secondary contaminated with Mg from the host serpentinite.
Název v anglickém jazyce
Tourmaline from Věžná I pegmatite; an indicator of external contamination and internal fractionation
Popis výsledku anglicky
Minerals of the tourmaline group are chemically very variable and therefore are good indicators of the degree of fractionation and pegmatite contamination. A typical example is the Věžná I locality. There were 6 types of tourmalines found in different zones of pegmatite. In the outer zones, Mg rich dravite predominates, replacing by schorl and foitite, and in the most fractionated parts by Mn and Li rich elbait and fluor-elbait. Tourmalines from more fractionated zones are secondary contaminated with Mg from the host serpentinite.

Rok uplatnění
2017
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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