http://www.cnr.it/ontology/cnr/individuo/prodotto/ID264199
On the symmetry and crystal structure of aguilarite, Ag4SeS. (Articolo in rivista)
- Type
- Label
- On the symmetry and crystal structure of aguilarite, Ag4SeS. (Articolo in rivista) (literal)
- Anno
- 2013-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1180/minmag.2013.077.1.03 (literal)
- Alternative label
Bindi L. [1, 2], Pingitore N. [3] (2013)
On the symmetry and crystal structure of aguilarite, Ag4SeS.
in Mineralogical magazine (Print); Mineralogical Society of Great Britain and Ireland, LONDON (Regno Unito)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Bindi L. [1, 2], Pingitore N. [3] (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
- http://minmag.geoscienceworld.org/ (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- [1] Dipartimento di Scienze della Terra, Universita` degli Studi di Firenze, Firenze, Italy
[2] CNR ? Istituto di Geoscienze e Georisorse, Sezione di Firenze, Firenze, Italy
[3] Department of Geological Sciences, The University of Texas at El Paso, El Paso, TX-79968-0555 Texas, USA (literal)
- Titolo
- On the symmetry and crystal structure of aguilarite, Ag4SeS. (literal)
- Abstract
- An examination of a specimen of aguilarite from the type locality provides new data on the chemistry
and structure of this mineral. The chemical formula of the crystal used for the structural study is
(Ag3.98Cu0.02)(Se0.98S0.84Te0.18), on the basis of 6 atoms. The mineral was found to be monoclinic,
crystallizing in space group P21/n, with a = 4.2478(2), b = 6.9432(3), c = 8.0042(5) A ? , b = 100.103(2)ยบ,
V = 232.41(2) A ? 3 and Z = 4. The crystal structure [refined to R1 = 0.0139 for 958 reflections with
I > 2s(I)] is topologically identical to that of acanthite, Ag2S. It can be described as a body-centred
array of tetrahedrally coordinated X atoms (X = S, Se and Te) with Ag2X3 triangles in planes nearly
parallel to (010); the sheets are linked by the Ag1 silver site, which has twofold coordination.
Aguilarite is definitively proved to be isostructural with acanthite; it does not have a naumannite-like
structure, as previously supposed. Our data support the hypothesis that there are two solid solution
series in the system: a monoclinic 'acanthite-like' series (from Ag2S?Ag2S0.4Se0.6), and an
orthorhombic 'naumannite-like' series (from Ag2S0.3Se0.7?Ag2Se). This is supported by data gathered
on synthetic counterparts. Aguilarite remains as a valid as a mineral species, but it should be described
as the Se-analogue of acanthite.
In this study we also (1) review the history of the aguilarite; (2) compare properties of synthetic and
natural aguilarite; and (3) demonstrate how earlier researchers erred in describing aguilarite as
orthorhombic.
The Te-bearing composition of the studied aguilarite crystal suggests the possibility of a solid
solution with cervelleite (Ag4TeS). (literal)
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