Chemistry:Caldasite

From HandWiki
Revision as of 22:30, 23 October 2022 by WikiEd2 (talk | contribs) (simplify)
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)
Caldasite
Zircon-favas[1]
Composition
PrimaryZircon (ZrSiO4), Baddeleyite (ZrO2)
SecondaryUranium (as triuranium octoxide [U2O3])

Caldasite (Portuguese: Caldasito, German: Zirkonglaskopf, Spanish: Caldasita)[1] is a rare uraniferous ore of zirconium found in the Poços de Caldas massif, located in the states of Minas Gerais and São Paulo, Brazil .

It is most often found as a dark gray, very dense, hard rock. It also appears as a friable brown substance.[2]

The massif is an alkaline complex, formed by a large intrusion during the mid-Cretaceous. The ore is a result of hydrothermal alteration of the nepheline-syenitic rocks; it has also been weathered out and concentrated in paleoplacer deposits.

References

  1. 1.0 1.1 Caldasite, MinDat.org, http://www.mindat.org/show.php?id=4714, retrieved January 30, 2016 
  2. Gonçalves, J.R.; Lakschevitz Jr., A. (August 1973) (in pt). Study of the mineral characteristics of caldasite. International Nuclear Information System. INIS-MF--1563. https://inis.iaea.org/search/search.aspx?orig_q=RN:5154997. Retrieved 8 February 2016. 

Further reading