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Reduction of symmetry in grandite solid solution

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dc.creator Galí Medina, Salvador, 1949-
dc.date 2011-05-25T10:48:45Z
dc.date 2011-05-25T10:48:45Z
dc.date 1984
dc.date.accessioned 2024-12-16T10:27:05Z
dc.date.available 2024-12-16T10:27:05Z
dc.identifier 0567-7505
dc.identifier http://hdl.handle.net/2445/18170
dc.identifier 80508
dc.identifier.uri http://fima-docencia.ub.edu:8080/xmlui/handle/123456789/21861
dc.description The results of a crystal structure refinement of an anisotropic grandite garnet specimen with composition Gro36-4 And63-6 are given. The structure obtained has orthorrombic symmetry (space group Fddd) and is compared with similar results obtained by other authors. In all cases the reduction of symmetry is due to the ordering of Fe3+ and Al in octahedral sites. Non cubic structures of grandites are discussed in connection with optical, morphological an grou-th features of these minerals.
dc.format 5 p.
dc.format application/pdf
dc.language eng
dc.publisher Universitat de Barcelona (UB). Institut de Cincias de la Terra Jaume Almera (ICTJA)
dc.relation Reproducció del document publicat a http://www.raco.cat/index.php/ActaGeologica/article/view/75177
dc.relation Acta Geologica Hispanica, 1984, vol. 19, num. 4, p. 287-293
dc.rights (c) Galí, 1984
dc.rights info:eu-repo/semantics/openAccess
dc.source Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)
dc.subject Estructura cristal·lina (Sòlids)
dc.subject Layer structure (Solids)
dc.title Reduction of symmetry in grandite solid solution
dc.type info:eu-repo/semantics/article
dc.type info:eu-repo/semantics/publishedVersion


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