Boron isotope variations in tourmaline from metacarbonates and associated calc-silicate rocks of the eastern part of the Bohemian Massif

Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216305%3A26110%2F17%3APU126835" target="_blank" >RIV/00216305:26110/17:PU126835 - 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
Boron isotope variations in tourmaline from metacarbonates and associated calc-silicate rocks of the eastern part of the Bohemian Massif
Popis výsledku v původním jazyce
Boron isotope variations in tourmaline from metacarbonates and associated calc-silicate rocks of the eastern part of the Bohemian Massif seem to be independent both on regional geological position and petrographic position within the rock. Boron isotope values largely overlap with the range of isotopic composition reported for crystalline rocks of the continental crust. Tourmaline signatures must be interpreted in the broader regional context of boron cycling in the Variscan orogeny.
Název v anglickém jazyce
Boron isotope variations in tourmaline from metacarbonates and associated calc-silicate rocks of the eastern part of the Bohemian Massif
Popis výsledku anglicky
Boron isotope variations in tourmaline from metacarbonates and associated calc-silicate rocks of the eastern part of the Bohemian Massif seem to be independent both on regional geological position and petrographic position within the rock. Boron isotope values largely overlap with the range of isotopic composition reported for crystalline rocks of the continental crust. Tourmaline signatures must be interpreted in the broader regional context of boron cycling in the Variscan orogeny.

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

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