Crystal chemistry of REEXO4 compounds (X = P, As, V). II. Review of REEXO4 compounds and their stability fields
- Autor(en)
- Uwe Kolitsch, D Holtstam
- Abstrakt
A comprehensive critical review of the phase fields, metastable
modifications, solid solution ranges and phase transitions of monazite-
and zircon-type REEXO4 (X = P, As, V) compounds is given. Monazite-type REEPO4,
compounds are stable for REE = La to Gd and metastable for Th to IIo;
zircon-type members exist for REE = Gd to Lu, and Y, Sc. REEAsO4,
compounds with monazite-type structure exist for REE = La to Nd, while
zircon-type compounds are known for REE = Pm to Lu, and Y, Sc; no
metastable arsenate members are known. The only stable monazite-type
REEVO4, is LaVO4, but metastable members are known for REE = Ce to Nd. Zircon-type REEVO4
compounds are stable for REE = Ce to Lu, and Y, Sc, and metastable for
REE = La. Solid solution series are complete only if minor size
differences exist between REE3+ or X5+ cations in
respective end-members. Phase transitions occur under pressure (zircon →
(monazite →)) scheelite) and at very low temperatures. The evaluation
of the metastable phase fields and of naturally occurring members
suggests that metastable modifications of REEXO4 compounds
can occur in nature under certain conditions (formation at temperatures
< ∼200-300°C; formation via hydrated precursor phases; stabilisation
by various impurity cations). © 2004 E. Schweizerbart'sche
Verlagsbuchhandlung, D-70176 Stuttgart.
- Organisation(en)
- Institut für Mineralogie und Kristallographie
- Externe Organisation(en)
- Swedish Museum of Natural History
- Journal
- European Journal of Mineralogy: an international journal of mineralogy, geochemistry and related sciences
- Band
- 16
- Seiten
- 117-126
- Anzahl der Seiten
- 10
- ISSN
- 0935-1221
- Publikationsdatum
- 2004
- Peer-reviewed
- Ja
- ÖFOS 2012
- 1051 Geologie, Mineralogie
- Link zum Portal
- https://ucrisportal.univie.ac.at/de/publications/2164c309-b0dc-40cd-a77d-d2cd6425c9b7