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dc.contributor.authorWeiss, Zdeněk
dc.contributor.authorRieder, Milan
dc.contributor.authorChmielová, Marta
dc.date.accessioned2007-11-19T09:46:28Z
dc.date.available2007-11-19T09:46:28Z
dc.date.issued1992
dc.identifier.citationEuropean Journal of Mineralogy. 1992, vol. 4, no. 4, p. 665-682.en
dc.identifier.issn0935-1221
dc.identifier.urihttp://hdl.handle.net/10084/64182
dc.language.isoenen
dc.publisherE. Schweizerbart'sche Verlagsbuchhandlungen
dc.relation.ispartofseriesEuropean Journal of Mineralogyen
dc.relation.urihttps://dx.doi.org/10.1127/ejm/4/4/0665en
dc.subjectpolyhedraen
dc.subjectdistortionsen
dc.subjectphyllosilicatesen
dc.subjectcrystal structuresen
dc.titleDeformation of coordination polyhedra and their sheets in phyllosilicatesen
dc.typearticleen
dc.identifier.locationNení ve fondu ÚKen
dc.description.abstract-enA statistical evaluation of crystal-structure data for 112 phyllosilicates (85 micas, 14 1 : 1 phyllosilicates, 13 chlorites) shows that the same principles govern the geometry of polyhedra and their sheets irrespective of the phyllosilicate subgroup. Regression relations for octahedral distortions and tetrahedral rotation as a function of interatomic distances are proposed. Multiple regressions were used to obtain generalized values for bond lengths and ionic radii for elements in different coordination. Using the relations derived here, it is possible to start with a chemical composition plus an anticipated cation ordering pattern and obtain estimates of the individual bond lengths and distortion characteristics of the crystal structure concerned. These can be translated into atomic coordinates and, ultimately, into peak intensities on diffraction patterns. The geometry of the coordination of interlayer cations in the micas shows considerable variation and the effective coordination number is seen to correlate with the tetrahedral rotation angle-alpha. When the coordination drops to six, this angle may vary between 16-degrees and 24-degrees.en
dc.identifier.doi10.1127/ejm/4/4/0665
dc.identifier.wosA1992JF89600002


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