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Campo Dublin Core | Valor | Idioma |
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dc.contributor.author | Menezes Filho, Luiz Alberto Dias | - |
dc.contributor.author | Atencio, Daniel | - |
dc.contributor.author | Andrade, Marcelo Barbosa de | - |
dc.contributor.author | Downs, Robert T. | - |
dc.contributor.author | Chaves, Mario Luiz de Sá Carneiro | - |
dc.contributor.author | Romano, Antônio Wilson | - |
dc.contributor.author | Persiano, Aba Israel Cohen | - |
dc.date.accessioned | 2017-07-24T13:20:59Z | - |
dc.date.available | 2017-07-24T13:20:59Z | - |
dc.date.issued | 2015 | - |
dc.identifier.citation | MENEZES FILHO, L. A. D. et al. Pauloabibite, trigonal NaNbO3, isostructural with ilmenite, from the Jacupiranga carbonatite, Cajati, São Paulo, Brazil. The American Mineralogist, v. 100, p. 442-446, 2015. Disponível em: <http://ammin.geoscienceworld.org/content/100/2-3/442>. Acesso em: 20 jun. 2017. | pt_BR |
dc.identifier.issn | 0003-004X | - |
dc.identifier.uri | http://www.repositorio.ufop.br/handle/123456789/8313 | - |
dc.description.abstract | Pauloabibite (IMA 2012-090), trigonal NaNbO3, occurs in the Jacupiranga carbonatite, in Cajati County, São Paulo State, Brazil, associated with dolomite, calcite, magnetite, phlogopite, pyrite, pyrrhotite, ancylite-(Ce), tochilinite, fluorapatite, “pyrochlore”, vigezzite, and strontianite. Pauloabibite occurs as encrustations of platy crystals, up to 2 mm in size, partially intergrown with an unidentified Ca-Nb-oxide, embedded in dolomite crystals, which in this zone of the mine can reach centimeter sizes. Cleavage is perfect on {001}. Pauloabibite is transparent and displays a sub-adamantine luster; it is pinkish brown and the streak is white. The calculated density is 4.246 g/cm3 . The mineral is uniaxial; n(mean)calc is 2.078. Chemical composition (n = 17, WDS, wt%) is: Na2O 16.36, MgO 0.04, CaO 1.36, MnO 0.82, FeO 0.11, SrO 0.02, BaO 0.16, SiO2 0.03, TiO2 0.86, Nb2O5 78.66, Ta2O5 0.34, total 98.76. The empirical formula is (Na0.88Ca0.04Mn2+ 0.02)S0.94(Nb0.98Ti0.02)S1.00O3. X-ray powder-diffraction lines (calculated pattern) [d in Å(I)(hkl)] are: 5.2066(100)(003), 4.4257(82)(101), 3.9730(45)(012), 2.9809(54) (104), 2.3718(88)(213), 1.9865(28)(024), 1.8620(53)(216), and 1.5383(30)(300). It is trigonal, space group: R3, a = 5.3287(5), c = 15.6197(17) Å, V = 384.10(7) Å3 , Z = 6. The crystal structure was solved (R1 = 0.0285, wR2 = 0.0636 for 309 observed reflections). Pauloabibite is isostructural with ilmenite and is polymorphic with isolueshite (cubic) and lueshite (orthorhombic). The name is in honor of Paulo Abib Andery (1922–1976). | pt_BR |
dc.language.iso | en_US | pt_BR |
dc.rights | restrito | pt_BR |
dc.subject | Pauloabibite | pt_BR |
dc.subject | New mineral | pt_BR |
dc.subject | Carbonatite | pt_BR |
dc.subject | Ilmenite structure | pt_BR |
dc.title | Pauloabibite, trigonal NaNbO3, isostructural with ilmenite, from the Jacupiranga carbonatite, Cajati, São Paulo, Brazil. | pt_BR |
dc.type | Artigo publicado em periodico | pt_BR |
dc.identifier.uri2 | http://ammin.geoscienceworld.org/content/100/2-3/442 | pt_BR |
dc.identifier.doi | https://doi.org/10.2138/am-2015-4745 | - |
Aparece nas coleções: | DEGEO - Artigos publicados em periódicos |
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