Carbonatite metasomatism overprinted by silicate melt metasomatism in the mantle beneath the West Eifel volcanic field

<p>The texture and mineral compositions of mantle xenoliths from the West Eifel volcanic field (WEVF) reveal three distinct mantle events. The first, identified in LREE-depleted and isotopically depleted anhydrous (type Ib) xenoliths, resulted from partial melting of fertile mantle around 2 Ga...

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Bibliographic Details
Main Authors: B. E. Bromley, S. Ma, C. S. J. Shaw
Format: Article
Language:English
Published: Copernicus Publications 2025-06-01
Series:European Journal of Mineralogy
Online Access:https://ejm.copernicus.org/articles/37/365/2025/ejm-37-365-2025.pdf
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