Articles | Volume 33, issue 5
https://doi.org/10.5194/ejm-33-605-2021
https://doi.org/10.5194/ejm-33-605-2021
Research article
 | 
06 Oct 2021
Research article |  | 06 Oct 2021

Authigenic rhabdophane from brown iron ore of the oxidation zone of the Babaryk massive sulfide occurrence (South Urals): scanning electron microscope (SEM) and electron backscattered diffraction (EBSD) study

Elena V. Belogub, Vladimir V. Shilovskikh, Konstantin A. Novoselov, Ivan A. Blinov, and Ksenia A. Filippova

Viewed

Total article views: 995 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
703 252 40 995 61 36 37
  • HTML: 703
  • PDF: 252
  • XML: 40
  • Total: 995
  • Supplement: 61
  • BibTeX: 36
  • EndNote: 37
Views and downloads (calculated since 06 Oct 2021)
Cumulative views and downloads (calculated since 06 Oct 2021)

Viewed (geographical distribution)

Total article views: 974 (including HTML, PDF, and XML) Thereof 974 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 08 Mar 2025
Download
Short summary
We found Ca- and S-rich rhabdophane in the upper part of the oxidation zone of a sulfide occurrence, where it forms spherules up to 35 µm in size and aggregates in fractures in goethite. Its formation is probably associated with desorption of REEs from Fe3+ oxyhydroxides and clay minerals in the oxidation zone and the influx of P from the soil as well as from the precursor rocks. The enrichment with REE phosphate in the studied case is similar to that in REE regolith-hosted deposits.
Share