Articles | Volume 36, issue 5
https://doi.org/10.5194/ejm-36-797-2024
https://doi.org/10.5194/ejm-36-797-2024
Research article
 | 
12 Sep 2024
Research article |  | 12 Sep 2024

Crystal chemistry of K-tourmalines from the Kumdy-Kol microdiamond deposit, Kokchetav Massif, Kazakhstan

Beatrice Celata, Ferdinando Bosi, Kira A. Musiyachenko, Andrey V. Korsakov, and Giovanni B. Andreozzi

Viewed

Total article views: 234 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
195 31 8 234 4 4
  • HTML: 195
  • PDF: 31
  • XML: 8
  • Total: 234
  • BibTeX: 4
  • EndNote: 4
Views and downloads (calculated since 12 Sep 2024)
Cumulative views and downloads (calculated since 12 Sep 2024)

Viewed (geographical distribution)

Total article views: 220 (including HTML, PDF, and XML) Thereof 220 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 20 Nov 2024
Download
Short summary
The discovery of the K-dominant tourmaline maruyamaite with microdiamond inclusions suggested its ultrahigh-pressure formation. We analyzed the role of K in the tourmaline structure, with a special focus on its stability. High pressure is necessary to squeeze the large cation K+ in the stiff framework of tourmaline, although K is the underdog component if Na+ is present in the mineralizing fluid. K-tourmaline is stable at high pressure, overcoming the stereotype of a mere crustal component.