Evolution of beryllium minerals in granitic pegmatite Maršíkov D6e, Czech Republic: Complex breakdown of primary beryl by internal and external hydrothermal-metamorphic fluids-Reference-Cited by-同舟云学术

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Evolution of beryllium minerals in granitic pegmatite Maršíkov D6e, Czech Republic: Complex breakdown of primary beryl by internal and external hydrothermal-metamorphic fluids

Published:2024-05 Issue:2 Volume:84 Page:126092
ISSN:0009-2819
Container-title:Geochemistry
language:en
Short-container-title:Geochemistry

Author:

Chládek Štěpán,Novák Milan,Uher Pavel,Gadas Petr,Matýsek Dalibor,Bačík Peter,Škoda Radek

Funder

Ministerstvo Školství, Mládeže a Tělovýchovy

Ministerstvo školstva, vedy, výskumu a športu Slovenskej republiky

Publisher

Elsevier BV

Reference78 articles.

1. Reappraisal of the crystal chemistry of beryl;Aurisicchio;Am. Mineral.,1988

2. Phase equilibria and thermodynamic properties of minerals in the BeO-Al2O3-SiO2-H2O (BASH) system, with petrologic applications;Barton;Am. Mineral.,1986

3. Non-pegmatitic deposits of beryllium: Mineralogy, geology, phase equilibria and origin;Barton,2002

4. Secondary blue tourmaline after garnet from elbaite-subtype pegmatites; implications for source and behavior of Ca and Mg in fluids;Buřival;J. Geosci.,2018

5. Subsolidus equilibria;Burt,1982

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