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'''Fergusonite''' is a mineral comprising a complex oxide of various rare earth elements. The chemical formula of fergusonite species is (Y,RE)NbO<sub>4</sub>, where RE = rare-earth elements in solid solution with Y. Yttrium is usually dominant (the species fergusonite-(Y)), but sometimes Ce or Nd may predominate in molar proportion (species fergusonite-(Ce) and fergusonite-(Nd)). All the other [[rare earth element]]s are present in subordinate amount, and [[tantalum]] substitutes for some of the [[niobium]]. There are [[Fergusonite-beta]]-(Nd), Fergusonite-beta-(Y), Fergusonite-beta-(Ce) too, but they are classified as 04.DG.10 in the [[Strunz classification|Nickel-Strunz]] system. The mineral has [[tetragonal]] crystal symmetry and the same structure as [[scheelite]] (calcium tungstate, CaW<sub>4</sub>), but can be [[metamict]] (amorphous) due to radiation damage from its small content of [[thorium]]. It is found as needle-like or prismatic crystals in [[pegmatite]]. It was named after British Politician and mineral collector [[Robert Ferguson of Raith]] (1767–1840)<ref>[http://www.scottish-places.info/people/famousfirst369.html University of Edinburgh]</ref>
'''Fergusonite''' is a mineral comprising a complex oxide of various rare earth elements. The chemical formula of fergusonite species is (Y,RE)NbO<sub>4</sub>, where RE = rare-earth elements in solid solution with Y. Yttrium is usually dominant (the species fergusonite-(Y)), but sometimes Ce or Nd may predominate in molar proportion (species fergusonite-(Ce) and fergusonite-(Nd)). All the other [[rare earth element]]s are present in subordinate amount, and [[tantalum]] substitutes for some of the [[niobium]]. There are [[Fergusonite-beta]]-(Nd), Fergusonite-beta-(Y), Fergusonite-beta-(Ce) too, but they are classified as 04.DG.10 in the [[Strunz classification|Nickel-Strunz]] system. The mineral has [[tetragonal]] crystal symmetry and the same structure as [[scheelite]] (calcium tungstate, CaWO<sub>4</sub>), but can be [[metamict]] (amorphous) due to radiation damage from its small content of [[thorium]]. It is found as needle-like or prismatic crystals in [[pegmatite]]. It was named after British Politician and mineral collector [[Robert Ferguson of Raith]] (1767–1840)<ref>[http://www.scottish-places.info/people/famousfirst369.html University of Edinburgh]</ref>


==See also==
==See also==

Revision as of 17:26, 13 September 2011

Fergusonite
General
CategoryOxide minerals
Formula
(repeating unit)
RENbO4 (RE=Rare earth)
Strunz classification07.GA.05
Crystal systemTetragonal - Dipyramidal (4/m) I 41/a
Identification
Formula mass245.81 (Y)
ColorBlack, Black, Brown, Gray, Yellow
Crystal habitMetamict - Mineral originally crystalline, now amorphous due to radiation damage
CleavageIndistinct
FractureSub Conchoidal - Fractures developed in brittle materials characterized by semi-curving surfaces
Mohs scale hardness5.5-6
LusterSub Metallic
Streakbrown
Density4.3 - 5.8, Average = 5.05
Refractive index2.05-2.19, isotropic
Other characteristicsNonmagnetic, Non-fluorescent, Not Radioactive
References[1]


Fergusonite is a mineral comprising a complex oxide of various rare earth elements. The chemical formula of fergusonite species is (Y,RE)NbO4, where RE = rare-earth elements in solid solution with Y. Yttrium is usually dominant (the species fergusonite-(Y)), but sometimes Ce or Nd may predominate in molar proportion (species fergusonite-(Ce) and fergusonite-(Nd)). All the other rare earth elements are present in subordinate amount, and tantalum substitutes for some of the niobium. There are Fergusonite-beta-(Nd), Fergusonite-beta-(Y), Fergusonite-beta-(Ce) too, but they are classified as 04.DG.10 in the Nickel-Strunz system. The mineral has tetragonal crystal symmetry and the same structure as scheelite (calcium tungstate, CaWO4), but can be metamict (amorphous) due to radiation damage from its small content of thorium. It is found as needle-like or prismatic crystals in pegmatite. It was named after British Politician and mineral collector Robert Ferguson of Raith (1767–1840)[2]

See also

References