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(2020) Concentration of REE-Nb-Zr-Be in the Baerzhe Deposit, NE China: Insights from Textural and Chemical Features of Amphibole and Rare Metal Minerals

Wu M, Samson I & Zhang D

https://doi.org/10.46427/gold2020.2895

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Submitted by Kathryn Watts on Thursday 25th June 19:29
Are the hypothesized immiscible F melts to source the late stage REE mineralization derived from fractional crystallization or some other process? What is the source of the F?
Thank you very much for your question. The generation of an immiscible fluoride melt should be regarded as magmatic processes. We believe that the Fluorine stemmed from the protoliths, as there is a lot of primary arfvedsonite in the granites

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