Articles | Volume 37, issue 1
https://doi.org/10.5194/ejm-37-39-2025
https://doi.org/10.5194/ejm-37-39-2025
Research article
 | 
20 Jan 2025
Research article |  | 20 Jan 2025

Dacostaite, K(Mg2Al)[Mg(H2O)6]2(AsO4)2F6  ⋅  2H2O, a new fluoride–arsenate mineral from the Cetine di Cotorniano Mine (Tuscany, Italy)

Cristian Biagioni, Daniela Mauro, Jiří Sejkora, Zdeněk Dolníček, Andrea Dini, and Radek Škoda

Viewed

Total article views: 218 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
172 39 7 218 19 5 2
  • HTML: 172
  • PDF: 39
  • XML: 7
  • Total: 218
  • Supplement: 19
  • BibTeX: 5
  • EndNote: 2
Views and downloads (calculated since 20 Jan 2025)
Cumulative views and downloads (calculated since 20 Jan 2025)

Viewed (geographical distribution)

Total article views: 231 (including HTML, PDF, and XML) Thereof 231 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 18 Apr 2025
Download
Short summary
Dacostaite is a new fluoride–arsenate mineral found in the Sb(Au) deposit of the Cetine di Cotorniano Mine (Tuscany, Italy). It shows a novel crystal structure formed by heteropolyhedral layers and isolated Mg(H2O)6 groups connected by H bonds. The heteropolyhedral layers are similar to those occurring in alunite-supergroup minerals, and this is a further example of the ability of nature to use similar modules in forming the large number of currently known structural arrangements. 
Share