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Parabariomicrolite discredited as identical to hydrokenomicrolite-3R

  • Daniel Atencio (a1)

Abstract

Proposal 16-C was accepted by the Commission on New Minerals and Mineral Names of the International Mineralogical Association, and parabariomicrolite is discredited as identical to hydrokenomicrolite-3R. There are now two type localities: Alto do Giz pegmatite, Equador Co., Rio Grande do Norte, Brazil and Volta Grande pegmatite, Nazareno, Minas Gerais, Brazil.

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Andrade, M.B., Atencio, D. Chukanov, N.V., and Ellena, J. (2013) Hydrokenomicrolite, (?,H2O)2Ta2(O,OH)6 (H2O), a new microlite-group mineral from Volta Grande pegmatite, Nazareno, Minas Gerais, Brazil. American Mineralogist, 98, 292296.
Ercit, T.S., Hawthorne, F.C. and ern, P. (1986) Parabariomicrolite, a new species, and its structural relationship to the pyrochlore group. The Canadian Mineralogist, 24, 655663.
Mills, S.J., Christy, A.G., Rumsey, M.S., and Spratt, J. (2016) The crystal chemistry of elsmoreite from the Hemerdon (Drakelands) mine, UK: Mineralogical Magazine, in press. doi:10.1180/minmag.2016.080.058.
Mumme, W.G., Grey, I.E., Birch, W.D., Pring, A., Bougerol, C., and Wilson, N.C. (2010) Coulsellite, CaNa3AlMg3F14, a rhombohedral pyrochlore with 1:3 ordering in both A and B sites, from the Cleveland Mine, Tasmania, Australia. American Mineralogist, 95, 736740.

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