Oxyyttropyrochlore-(Y),[1] also referred to as "obruchevite" or "yttropyrochlore-(Y)", is a potential (not yet accepted) zero-valent-dominant mineral of the pyrochlore group. Its formula can be written as (Y,◻)2Nb2O2O.
The name "yttropyrochlore-(Y)" for this compound was used by Kalita (1957), and Ercit et al. (2003), but it has become obsolete and the mineral status is not yet clear. The yttropyrochlore-(Y) as mentioned by Tindle & Breaks (1998) is in fact "oxyyttropyrochlore-(Y)".
References
edit- Atencio, Daniel; Andrade, Marcelo B.; Christy, Andrew G.; Gieré, Reto; Kartashov, Pavel M. (2010). "The Pyrochlore Supergroup of Minerals: Nomenclature" (PDF). The Canadian Mineralogist. pp. 673–698. Archived from the original (PDF) on 2012-03-26. Retrieved 2013-12-02. Citing:
- Ercit, T.S.; Groat, L.A.; Gault, R.A. (2003). "Granitic pegmatites of the O'Grady batholith, N.W.T., Canada: a case study of the evolution of the elbaite subtype of rare-element granitic pegmatite". The Canadian Mineralogist. 41: 117–137. doi:10.2113/gscanmin.41.1.117.
- Kalita, A.P. (1957). "On the composition of obruchevite – a hydrated uranium–yttrium variety of pyrochlore". Doklady Akademii Nauk SSSR (in Russian). 117: 117–120.
- Tindle, A.G.; Breaks, F.W. (1998). "Oxide minerals of the Separation Rapids rare-element granitic pegmatite group, northwestern Ontario". The Canadian Mineralogist. 36: 609–635.
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