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(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

Pauloabibite, trigonal NaNbO3, isostructural with ilmenite, from the Jacupiranga carbonatite, Cajati, Sao Paulo, Brazil

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Author(s):
Menezes Filho, Luiz A. D. [1] ; Atencio, Daniel [2] ; Andrade, Marcelo B. [3] ; Downs, Robert T. [4] ; Chaves, Mario L. S. C. [1] ; Romano, Antonio W. [1] ; Scholz, Ricardo [5] ; Persiano, Aba I. C. [6]
Total Authors: 8
Affiliation:
[1] Univ Fed Minas Gerais, Inst Geociencias, BR-31270901 Belo Horizonte, MG - Brazil
[2] Univ Sao Paulo, Inst Geociencias, BR-05508080 Sao Paulo, SP - Brazil
[3] Univ Sao Paulo, Inst Fis Sao Carlos, BR-13560970 Sao Carlos, SP - Brazil
[4] Univ Arizona, Dept Geosci, Tucson, AZ 85721 - USA
[5] Univ Fed Ouro Preto, Escola Minas, Dept Geol, BR-35400000 Ouro Preto, MG - Brazil
[6] Univ Fed Minas Gerais, Inst Ciencias Exatas, Dept Fis, BR-31279901 Belo Horizonte, MG - Brazil
Total Affiliations: 6
Document type: Journal article
Source: AMERICAN MINERALOGIST; v. 100, n. 2-3, p. 442-446, FEB-MAR 2015.
Web of Science Citations: 8
Abstract

Pauloabibite (IMA 2012-090), trigonal NaNbO3, occurs in the Jacupiranga carbonatite, in Cajati County, Sao 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/cm(3). 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 (Na0.88Ca0.04Mn0.022+)Sigma(0.94)(NID0.98Ti0.02)(Sigma 1.00)O-3. X-ray powder-diffraction lines (calculated pattern) {[}d in angstrom(I)(hkl)] are: 5.2066(100)(003), 4.4257(82)(101), 3.9730(45)(012), 2.9809(54) (104), 2.3718(88)(2 (1) over bar3), 1.9865(28)(024), 1.8620(53)(2 (1) over bar6), and 1.5383(30)(300). It is trigonal, space group: R (3) over bar, a = 5.3287(5), c = 15.6197(17) angstrom, Z = 384.10(7) angstrom(3), Z = 6. The crystal structure was solved (R-1 = 0.0285, wR(2) = 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). (AU)

FAPESP's process: 11/22407-0 - New and rare Brazilian mineral species characterization
Grantee:Daniel Atencio
Support Opportunities: Regular Research Grants
FAPESP's process: 13/03487-8 - Center of characterization of new mineral species: Raman spectroscopy, electron microprobe and X-ray and neutron diffraction
Grantee:Marcelo Barbosa de Andrade
Support Opportunities: Research Grants - Young Investigators Grants