Hostname: page-component-cd9895bd7-mkpzs Total loading time: 0 Render date: 2024-12-26T06:10:39.819Z Has data issue: false hasContentIssue false

Oxycalciomicrolite, (Ca,Na)2(Ta,Nb,Ti)2O6(O,F), a new member of the microlite group (pyrochlore supergroup) from the Paleoproterozoic São João del Rei Pegmatite Province, Minas Gerais state, Brazil

Published online by Cambridge University Press:  25 September 2020

Victor H.R. Menezes da Silva*
Affiliation:
Programa de Pós-Graduação em Geologia, Instituto de Geociências, Universidade Federal do Rio de Janeiro, Cidade Universitária, 21949-900, Ilha do Fundão, Rio de Janeiro, RJ, Brazil
Ciro A. Ávila
Affiliation:
Programa de Pós-Graduação em Geologia, Instituto de Geociências, Universidade Federal do Rio de Janeiro, Cidade Universitária, 21949-900, Ilha do Fundão, Rio de Janeiro, RJ, Brazil Departamento de Geologia e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro, Quinta da Boa Vista s/n, 20940-040, São Cristóvão, Rio de Janeiro, RJ, Brazil
Reiner Neumann
Affiliation:
Departamento de Geologia e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro, Quinta da Boa Vista s/n, 20940-040, São Cristóvão, Rio de Janeiro, RJ, Brazil CETEM – Centro de Tecnologia Mineral, Setor de Caracterização Tecnológica, Avenida Pedro Calmon, 900, 22941-908, Ilha do Fundão, Rio de Janeiro, RJ, Brazil
Fabiano R.L. Faulstich
Affiliation:
Departamento de Geologia e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro, Quinta da Boa Vista s/n, 20940-040, São Cristóvão, Rio de Janeiro, RJ, Brazil
Felipe E.A. Alves
Affiliation:
Programa de Pós-Graduação em Geologia, Instituto de Geociências, Universidade Federal do Rio de Janeiro, Cidade Universitária, 21949-900, Ilha do Fundão, Rio de Janeiro, RJ, Brazil
Filipe B. de Almeida
Affiliation:
Instituto de Química, Universidade Federal Fluminense, Rua Outeiro de São João Batista, s/n°, 24020-141, Campus do Valonguinho, Niterói, RJ, Brazil
Tais Proença Cidade
Affiliation:
CETEM – Centro de Tecnologia Mineral, Setor de Caracterização Tecnológica, Avenida Pedro Calmon, 900, 22941-908, Ilha do Fundão, Rio de Janeiro, RJ, Brazil
Sarah Siqueira da Cruz Guimarães Sousa
Affiliation:
Programa de Pós-Graduação em Geologia, Instituto de Geociências, Universidade Federal do Rio de Janeiro, Cidade Universitária, 21949-900, Ilha do Fundão, Rio de Janeiro, RJ, Brazil Departamento de Geologia e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro, Quinta da Boa Vista s/n, 20940-040, São Cristóvão, Rio de Janeiro, RJ, Brazil
*
*Author for correspondence: Victor H.R. Menezes da Silva, Email: vmenezes92@gmail.com

Abstract

Oxycalciomicrolite (IMA2019-110), (Ca,Na)2(Ta,Nb,Ti)2O6(O,F), is a new member of microlite-group mineral found in the saprolite of the weathered Fumal pegmatite, located close to the city of Nazareno, Minas Gerais state, Brazil. It occurs as an accessory mineral associated with quartz, albite, microcline, muscovite, columbite-subgroup minerals, cassiterite, hematite, ilmenite, monazite-(Ce), xenotime-(Y), zircon, beryl, spinel, epidote and garnet-group minerals. Oxycalciomicrolite is found as octahedral crystals, occasionally modified to rhombododecahedra, ranging from 0.2 to 0.5 mm in size. The crystals are brownish-yellow to brownish-red and translucent, with white streak and vitreous to resinous lustre. The tenacity is brittle, with a Mohs hardness of 5–5½. Cleavage and parting are not observed; the fracture is conchoidal. Electron microprobe analysis, Raman and infrared spectroscopies and X-ray powder diffraction were applied to characterise this mineral. Oxycalciomicrolite is isotropic, ncalc. = 2.037, and the calculated density is 6.333 g/cm3. The composition is (Ca1.570.26Na0.06Sn0.03Sr0.03U0.02Mn0.02Fe0.01Ce0.01)∑2.00(Ta1.79Nb0.18Ti0.03)∑2.00O6.00[O0.64F0.190.17]∑1.00 analysed by electron microprobe using wavelength dispersive spectrometry. The unit-cell parameters obtained by Pawley fitting from powder X-ray diffraction data are a = 10.4325(4) Å and V = 1135.46(14) Å3 with Z = 8.

Type
Article
Copyright
Copyright © The Author(s), 2020. Published by Cambridge University Press on behalf of The Mineralogical Society of Great Britain and Ireland

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Footnotes

Associate Editor: Sergey V. Krivovichev

References

Alves, F.E.A., Neumann, R., Ávila, C.A. and Faulstich, F.R.L. (2019) Monazite-(Ce) and xenotime-(Y) microinclusions in fluorapatite of the pegmatites from the Volta Grande mine, Minas Gerais state, southeast Brazil, as witnesses of dissolution-reprecipitation process. Mineralogical Magazine, 83, 595606.CrossRefGoogle Scholar
Andrade, M.B., Atencio, D., Chukanov, N.V. and Ellena, J. (2013a) Hydrokenomicrolite, (□,H2O)2Ta2(O,OH)6(H2O), a new microlite-group mineral from Volta Grande pegmatite, Nazareno, Minas Gerais, Brazil. American Mineralogist, 98, 292296.CrossRefGoogle Scholar
Andrade, M.B., Atencio, D., Persiano, A.I.C. and Ellena, J. (2013b) Fluorcalciomicrolite, (Ca,Na,□)2Ta2O6F, a new microlite-group mineral from Volta Grande pegmatite, Nazareno, Minas Gerais, Brazil. Mineralogical Magazine, 77, 29892996.CrossRefGoogle Scholar
Andrade, M.B., Yang, H., Atencio, D., Downs, R.T., Chukanov, N.V., Lemée-Cailleau, M.H., Persiano, A.I.C., Goeta, A.E. and Ellena, J. (2017) Hydroxycalciomicrolite, Ca1.5Ta2O6(OH), a new member of the microlite group from Volta Grande pegmatite, Nazareno, Minas Gerais, Brazil. Mineralogical Magazine, 81, 555564.CrossRefGoogle Scholar
Arenas, D.J., Gasparov, L.V., Wei Qiu Nino, J.C., Patterson, C.H. and Tanner, D.B. (2010) Raman study of phonon modes in bismuth pyrochlores. The American Physical Society, 82, 214302.Google Scholar
Atencio, D., Andrade, M.B., Christy, A.G., Gieré, R. and Kartashov, P.M. (2010) The pyrochlore supergroup of minerals nomenclature. The Canadian Mineralogist, 48, 673698.CrossRefGoogle Scholar
Atencio, D., Andrade, M.B., Bastos Neto, A.C. and Pereira, V.P. (2017) Ralstonite renamed hydrokenoalstonite, coulsellite renamed fluornatrocoulsellite, and their incorporations into the pyrochlore supergroup. The Canadian Mineralogist, 55, 115120.CrossRefGoogle Scholar
Ávila, C.A., Teixeira, W., Cordani, U.G., Moura, C.A.V. and Pereira, R.M., (2010) Rhyacian (2.23–2.20 Ga) juvenile accretion in the southern São Francisco craton, Brazil: Geochemical and isotopic evidence from the Serrinha magmatic suite, Mineiro belt. Journal of South American Earth Sciences, 29, 464482.CrossRefGoogle Scholar
Ávila, C.A., Teixeira, W., Bongiolo, E.M., Dussin, I.A., and Vieira, T.A.T. (2014) Rhyacian evolution of subvolcanic and metasedimentary rocks of the southern segment of the Mineiro belt, São Francisco Craton, Brazil. Precambrian Research, 243, 221251.CrossRefGoogle Scholar
Bahfenne, S. and Frost, R.L. (2010) Raman spectroscopic study of the antimonate mineral roméite. Spectrochimica Acta Part A, 75, 637639.CrossRefGoogle ScholarPubMed
Biagioni, C., Orlandi, P., Nestola, F. and Bianchin, S. (2013) Oxycalcioroméite, Ca2Sb2O6O, from Buca della Vena mine, Apuan Als, Tuscany, Italy: a new member of the pyrochlore supergroup. Mineralogical Magazine, 77, 30273037.CrossRefGoogle Scholar
Bosi, F., Hatert, F., Hålenius, U., Pasero, M., Miyawaki, R. and Mills, S.J. (2019) On the application of the IMA-CNMNC dominant-valency rule to complex mineral compositions. Mineralogical Magazine, 83, 627632.CrossRefGoogle Scholar
Brugger, J., Gieré, R., Graeser, S. and Meisser, N. (1997) The crystal chemistry of roméite. Contributions to Mineralogy and Petrology, 127, 136146.CrossRefGoogle Scholar
Černý, P., Chapman, R., Ferreira, K. and Smeds, S.A. (2004) Geochemistry of oxide minerals of Nb, Ta, Sn and Sb in the Varuträsk granitic pegmatite, Sweden: the case of an “anomalous” columbite–tantalite trend. American Mineralogist, 89, 505588.CrossRefGoogle Scholar
Ercit, T.S. and Robinson, G.W. (1994) A refinement of the structure of ferritungstite from Kalzas Mountain, Yukon, and observation on the tungsten pyrochlores. The Canadian Mineralogist, 32, 567574.Google Scholar
Faulstich, F.R.L. (2016) Study of heavy minerals from pegmatites of São João del Rei Pegmatitic Province, Minas Gerais. DSc thesis. Instituto de Geociências, Universidade Federal do Rio de Janeiro, Brazil.Google Scholar
Glerup, M., Nielsen, O.F. and Poulsen, F.W. (2001) The structural transformation from the pyrochlore structure, A 2B 2O7, to the fluorite structure, AO2, studied by Raman spectroscopy and defect chemistry modeling. Journal of Solid State Chemistry, 160, 2532.CrossRefGoogle Scholar
Guang, Fan., Ge, Xiangkun., Li, Guowu., Yu, Apeng. and Shen, Ganfu. (2017) Oxynatromicrolite, (Na,Ca,U)2Ta2O6(O,F), a new member of the pyrochlore supergroup from Guanpo, Henan Province, China. Mineralogical Magazine, 81, 743751.CrossRefGoogle Scholar
Guastoni, A., Diela, V. and Pezzotta, F. (2008) Vigezzite and associated oxides of Nb–Ta from emerald-bearing pegmatites of the Vigezzo Valley, Western Alps, Italy. The Canadian Mineralogist, 46, 619633.CrossRefGoogle Scholar
Hogarth, D.D. (1977) Classification and nomenclature of the pyrochlore group. American Mineralogist, 6, 610633.Google Scholar
Lagache, M. and Quéméneur, J. (1997) The Volta Grande pegmatites, Minas Gerais, Brazil: an example of rare-element granitic pegmatites exceptionally enriched in lithium and rubidium. The Canadian Mineralogist, 35, 153165.Google Scholar
Lumpkin, G.R. and Ewing, R.C. (1992) Geochemical alteration of pyrochlore group minerals: microlite subgroup. American Mineralogist, 77, 179188.Google Scholar
Lumpkin, G.R. and Ewing, R.C. (1995) Geochemical alteration of pyrochlore group minerals: pyrochlore subgroup. American Mineralogist, 80, 732743.CrossRefGoogle Scholar
Mandarino, J.A. (1981) The Gladstone – Dale Relationship: Part IV. The compatibility concept and its application. The Canadian Mineralogist, 19, 441450.Google Scholar
Menezes da Silva, V.H.R., Neumann, R., Ávila, C.A., Faulstich, F.R.L., Alves, F.E.A. and de Almeida, F.B. (2020) Oxycalciomicrolite, IMA 2019-110. CNMNC Newsletter No. 54; Mineralogical Magazine, 84, 359365, https://doi.org/10.1180/mgm.2020.21Google Scholar
Pereira, R.M., Ávila, C.A., Neumann, R., Netto, A.M. and Atencio, D. (2003) Edge of zirconiferous hafnon in hafniferous zircon of the Volta Grande mine, São João del Rei pegmatitic province, Minas Gerais, Brazil. Boletim do Museu Nacional, Geology Series, 69, 114.Google Scholar
Teixeira, W., Ávila, C.A., Dussin, I. A., Corrêa Neto, A.V., Bongiolo, E.M., Santos, J.O. and Barbosa, N.S. (2015) A juvenile accretion episode (2.35–2.32 Ga) in the Mineiro belt and its role to the Minas accretionary orogeny: Zircon U–Pb–Hf and geochemical evidences. Precambrian Research, 256, 148169.CrossRefGoogle Scholar