To use all functions of this page, please activate cookies in your browser.
With an accout for my.chemeurope.com you can always see everything at a glance – and you can configure your own website and individual newsletter.
- My watch list
- My saved searches
- My saved topics
- My newsletter
Baddeleyite is a rare zirconium oxide mineral (ZrO2 or zirconia), occurring in a variety of monoclinic prismatic crystal forms. It is transparent to translucent, has high indices of refraction (nα=2.130, nβ=2.190, and nγ=2.200), and ranges from colorless to yellow, green, and dark brown. The mineral has a specific gravity of 5.5 to 6 and a Mohs hardness of 6.5. Baddeleyite is a refractory mineral, with a melting point of 2700 °C. Hafnium is a substituting impurity and may be present in quantities ranging from 0.1 to several percent.
Baddeleyite was first described in 1892 from Sri Lanka, and Minas Gerais and Jacupiranga, São Paulo, Brazil. It was named after Joseph Baddeley, who described the occurrences in Sri Lanka.
Baddeleyete is often found as detrital grains in gravels. Its primary occurrence is in high temperature veins and in syenite, carbonatite, kimberlite, and lamproite intrusions. Because of their refractory nature and stability under diverse conditions, baddeleyete grains, along with zircon, are used for uranium-lead radiometric age determinations.
|This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Baddeleyite". A list of authors is available in Wikipedia.|