Abellaite, NaPb2(CO3)2(OH), a new supergene mineral from the Eureka mine, Lleida province, Catalonia, Spain

dc.contributor.author
Ibáñez i Insa, Jordi
dc.contributor.author
Elvira, José J.
dc.contributor.author
Llovet Ximenes, Xavier
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Pérez Cano, Jordi
dc.contributor.author
Oriols, Núria
dc.contributor.author
Busquets Masó, Martí
dc.contributor.author
Hernández Márquez, Sergi
dc.date.issued
2018-11-19T10:23:29Z
dc.date.issued
2018-11-19T10:23:29Z
dc.date.issued
2017-03-30
dc.date.issued
2018-11-19T10:23:29Z
dc.identifier
0935-1221
dc.identifier
https://hdl.handle.net/2445/126204
dc.identifier
670806
dc.description.abstract
The new mineral abellaite (IMA 2014-111), ideally NaPb2 (CO3)2 (OH), is a supergene mineral that was found in one of the galleries of the long-disused Eureka mine, in the southern Pyrenees (Lleida province), Catalonia, Spain. Abellaite is found as sparse coatings on the surface of the primary mineralization, it forms subhedral crystals not larger than 10μm as well as larger pseudohexagonal platelets up to ~ 30μm. Individual crystals commonly have a tabular to lamellar habit and form fairly disordered aggregates. The mineral is associated with a large number of primary minerals (roscoelite, pyrite, uraninite, coffinite, 'carbon', galena, sphalerite, nickeloan cobaltite, covellite, tennantite and chalcopyrite) and supergene minerals (hydrozincite, aragonite, gordaite, As-rich vanadinite andersonite, čejkaite, malachite and devilline). Abellaite is colourless to white, with a vitreous to nacreous lustre. The mineral is translucent, has a white streak and is non-fluorescent. The aggregates of microcrystals are highly friable. The calculated density using the ideal formula is 5.93 g/cm3. The chemical composition of the mineral (the mean of 10 electron microprobe analyses) is Na 3.88, Ca 0.29, Pb 72.03, C 4.17, O 19.47 and H 0.17, total 100.00 wt% (H, C and O by stoichiometry assuming the ideal formula). On the basis of 7 O atoms, the empirical formula of abellaite is Na0.96 Ca0.04 Pb1.98 (CO3)2 (OH). The simplified formula of the mineral is NaPb2 (CO3)2 (OH). The mineral is hexagonal, space group P 63 mc, a = 5.254(2), c = 13.450(5) Å, V = 321.5(2) Å3 and Z = 2. The strongest powder-diffraction lines [d in Å (I) (h k l)] are: 3.193 (100) (0 1 3), 2.627 (84) (1 1 0), 2.275 (29) (0 2 0), 2.242 (65) (0 2 1, 0 0 6), 2.029(95) (0 2 3). Abellaite has a known synthetic analogue, and the crystal structure of the mineral was refined by using crystallographic data of the synthetic phase. The mineral is named in honour of the mineralogist and gemmologist Joan Abella i Creus (b. 1968), who has long studied the deposits of the Eureka mine and who collected the mineral.
dc.format
27 p.
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application/pdf
dc.format
application/pdf
dc.language
eng
dc.publisher
Schweizerbart
dc.relation
Versió postprint del document publicat a: https://doi.org/10.1127/ejm/2017/0029-2630
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European Journal of Mineralogy, 2017, vol. 29, num. 5, p. 915-922
dc.relation
https://doi.org/10.1127/ejm/2017/0029-2630
dc.rights
(c) Schweizerbart, 2017
dc.rights
info:eu-repo/semantics/openAccess
dc.source
Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)
dc.subject
Mineralogia
dc.subject
Carbonats
dc.subject
Mineralogy
dc.subject
Carbonates
dc.title
Abellaite, NaPb2(CO3)2(OH), a new supergene mineral from the Eureka mine, Lleida province, Catalonia, Spain
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/acceptedVersion


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