Rankamaite from the Urubu pegmatite, Itinga, Minas Gerais, Brazil: Crystal chemistry and Rietveld refinement


Autoria(s): Atencio, Daniel; CONTREIRA FILHO, Reynaldo R.; MILLS, Stuart J.; Coutinho, Jose Moacyr Vianna; HONORATO, Sara B.; AYALA, Alejandro P.; ELLENA, Javier; ANDRADE, Marcelo B. de
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

20/10/2012

20/10/2012

2011

Resumo

A new occurrence of rankamaite is here described at the Urubu pegmatite, Itinga municipality, Minas Gerais, Brazil. The mineral forms cream-white botryoidal aggregates of acicular to fibrous crystals, intimately associated with simpsonite, thoreaulite, cassiterite, quartz, elbaite, albite, and muscovite. The average of six chemical analyses obtained by electron microprobe is (range in parentheses, wt%): Na(2)O 2.08 (1.95-2.13), K(2)O 2.61 (2.52-2.74), Al(2)O(3) 1.96 (1.89-2.00), Fe(2)O(3) 0.01 (0.00-0.03), TiO(2) 0.02 (0.00-0.06), Ta(2)O(5) 81.04 (79.12-85.18), Nb(2)O(5) 9.49 (8.58-9.86), total 97.21 (95.95-101.50). The chemical formula derived from this analysis is (Na(1.55)K(1.28))(Sigma 2.83)(Ta(8.45)Nb(1.64)Al(0.89)Fe(0.01)(3+)Ti(0.01))(Sigma 11.00)[O(25.02)(OH)(5.98)](Sigma 31.00). Rankamaite is an orthorhombic ""tungsten bronze"" (OTB), crystallizing in the space group Cmmm. Its unit-cell parameters refined from X-ray diffraction powder data are: a = 17.224(3), b = 17.687(3), c = 3.9361(7) angstrom, V = 1199.1(3) angstrom(3), Z = 2. Rietveld refinement of the powder data was undertaken using the structure of LaTa(5)O(14) as a starting model for the rankamaite structure. The structural formula obtained with the Rietveld analyses is: (Na(2.21)K(1.26))Sigma(3.37)(Ta(9.12)NB(1.30) Al(0.59))(Sigma 11.00)[O(26.29)(OH)(4.71)](Sigma 31.00). The tantalum atoms are coordinated by six and seven oxygen atoms in the form of distorted TaO(6) octahedra and TaO(2) pentagonal bipyramids, respectively. Every pentagonal bipyramid shares edges with four octahedra, thus forming Ta(5)O(14) units. The potassium atom is in an 11-fold coordination, whereas one sodium atom is in a 10-fold and the other is in a 12-fold coordination. Raman and infrared spectroscopy were used to investigate the room-temperature spectra of rankamaite.

FAPESP[2008/04984-7]

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

FAPESP[2009/09125-5]

Identificador

AMERICAN MINERALOGIST, v.96, n.10, p.1455-1460, 2011

0003-004X

http://producao.usp.br/handle/BDPI/30213

10.2138/am.2011.3594

http://dx.doi.org/10.2138/am.2011.3594

Idioma(s)

eng

Publicador

MINERALOGICAL SOC AMER

Relação

American Mineralogist

Direitos

restrictedAccess

Copyright MINERALOGICAL SOC AMER

Palavras-Chave #Rankamaite #tungsten bronze #tantalate #Unibu pegmatite #Itinga #Minas Gerais #Brazil #Rietveld refinement #GRANITE PEGMATITES #RAMAN-SCATTERING #PENTOXIDE #CERAMICS #TANTALUM #NIOBIUM #Geochemistry & Geophysics #Mineralogy
Tipo

article

original article

publishedVersion