Articles | Volume 37, issue 3
https://doi.org/10.5194/ejm-37-365-2025
https://doi.org/10.5194/ejm-37-365-2025
Research article
 | 
30 Jun 2025
Research article |  | 30 Jun 2025

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

Beatrice E. Bromley, Shuai Ma, and Cliff S. J. Shaw

Viewed

Total article views: 1,765 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,291 369 105 1,765 57 100 155
  • HTML: 1,291
  • PDF: 369
  • XML: 105
  • Total: 1,765
  • Supplement: 57
  • BibTeX: 100
  • EndNote: 155
Views and downloads (calculated since 30 Jun 2025)
Cumulative views and downloads (calculated since 30 Jun 2025)

Viewed (geographical distribution)

Total article views: 1,701 (including HTML, PDF, and XML) Thereof 1,701 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 01 Oct 2026
Download
Short summary
Understanding the chemical evolution of the earth's mantle is important in the cycling of elements through the earth system. This work shows how mantle that has previously been partially melted can be re-enriched by carbonate-rich and silicate magmas. Samples of the mantle collected from volcanic rocks in the Eifel volcanic field and the mineral clinopyroxene were analyzed to reveal its chemical signatures, which were used to determine the nature of the processes that affected the Eifel mantle.
Share