Caldasite Explained

Caldasite
Alternative Name:Zircon-favas
Composition:Zircon (ZrSiO4), Baddeleyite (ZrO2)
Composition Secondary:Uranium (as triuranium octoxide [U<sub>2</sub>O<sub>3</sub>])

Caldasite 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.[1]

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.

Further reading

Notes and References

  1. Gonçalves. J.R.. Lakschevitz Jr.. A.. Study of the mineral characteristics of caldasite. INIS. International Nuclear Information System. 8 February 2016. pt. August 1973 . INIS-MF--1563.