Formation of the Lened W-(Be) Skarn Deposit by Neutralization of a Magmatic Fluid—Evidence from H<sub>3</sub>BO<sub>3</sub>-Rich Fluids

Formation of the Lened W-(Be) Skarn Deposit by Neutralization of a Magmatic Fluid—Evidence from H<sub>3</sub>BO<sub>3</sub>-Rich Fluids

Magmatic-hydrothermal systems, especially those causing the formation of tungsten deposits, may be enriched in boron, as is suggested by the presence of hydrothermal tourmaline. This study examines the boron and metal (including tungsten) concentrations of quartz-hosted fluid inclusions in the Lened...

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Bibliographic Details
Main Authors: Hélène Legros, Vanessa Elongo, Oscar Laurent, Erin Adlakha, Cyril Chelle-Michou, Hendrik Falck, Pilar Lecumberri-Sanchez
Format: Article
Language:English
Published: MDPI AG 2022-06-01
Series:Geosciences
Subjects:
fluid inclusion
sassolite
Lened
boron
emerald
scheelite
Online Access:https://www.mdpi.com/2076-3263/12/6/236

Internet

https://www.mdpi.com/2076-3263/12/6/236

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