The effect of fluorine on mineral-carbonatitic melt partitioning of trace elements – Implications for critical mineral deposits-Reference-Cited by-同舟云学术

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The effect of fluorine on mineral-carbonatitic melt partitioning of trace elements – Implications for critical mineral deposits

Published:2024-08 Issue: Volume:379 Page:53-75
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Xue Shuo,Dasgupta Rajdeep^ORCID,Ling Ming-Xing,Sun Weidong^ORCID,Lee Cin-Ty A.

Publisher

Elsevier BV

Reference135 articles.

1. Experimentally determined partition coefficients for minor and trace elements in peridotite minerals and carbonatitic melt, and their relevance to natural carbonatites;Adam;Eur. J. Mineral.,2001

2. Formation of rare earth deposits in carbonatites;Anenburg;Elements,2021

3. Silica is unlikely to be soluble in upper crustal carbonatite melts;Anenburg;Nat. Commun.,2023

4. Rare earth element mobility in and around carbonatites controlled by sodium, potassium, and silica;Anenburg;Sci. Adv.,2020

5. Rare earth element deposits: Sources, and exploration strategies;Balaram;J. Geol. Soc. India,2022

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