| dc.contributor.author | Weiss, Zdeněk | |
| dc.contributor.author | Rieder, Milan | |
| dc.contributor.author | Smrčok, Ľubomír | |
| dc.contributor.author | Petříček, Václav | |
| dc.contributor.author | Bailey, Sturges W. | |
| dc.date.accessioned | 2007-11-14T09:25:18Z | |
| dc.date.available | 2007-11-14T09:25:18Z | |
| dc.date.issued | 1993 | |
| dc.identifier.citation | European Journal of Mineralogy. 1993, vol. 5, no. 3, p. 493-502. | en |
| dc.identifier.issn | 0935-1221 | |
| dc.identifier.uri | http://hdl.handle.net/10084/64094 | |
| dc.language.iso | en | en |
| dc.publisher | E. Schweizerbart'sche Verlagsbuchhandlung | en |
| dc.relation.ispartofseries | European Journal of Mineralogy | en |
| dc.relation.uri | https://dx.doi.org/10.1127/ejm/5/3/0493 | en |
| dc.subject | mica | en |
| dc.subject | crystal structure | en |
| dc.subject | cation ordering | en |
| dc.subject | polytypism | en |
| dc.title | Refinement of the crystal structures of two "protolithionites" | en |
| dc.type | article | en |
| dc.identifier.location | Není ve fondu ÚK | en |
| dc.description.abstract-en | Crystal structures of "protolithionites" 1M and 3T were refined in the C2/m and P3(1)12 space groups with R equal to 3.8 and 3.0 % and R(w) 5.4 and 3.2 %, respectively. Refinement of the 1M structure in subgroup symmetry (C2) did not result in a significant improvement of fit and was not accepted. The 1 M mica has a mesooctahedral cation ordering (two octahedra identical), similar to that of muscovite but with less pronounced differences in size between M1 and M2 ; Li and Fe2+ prefer M1 to M2, Al does the opposite. Like all 3T structures refined to date, the "prototithionite" 3T has a heterooctahedral ordering rather similar to that found in "protolithionite" 3T of Pavlishin et al. (1981) and zinnwaldite 1M of Guggenheim & Bailey (1977), The two large (though not identical) octahedra M3, M1 contain all Li and most Fe, the small (M2) octahedron is occupied with Al. This type of ordering is apparently suitable for a relatively wide range of compositions of Li-Fe micas; the lepidolites are not included, and neither are iron-rich compositions. "Protolithionite" 1M has no pronounced octahedral ordering and all octahedra are nearly the same in size. | en |
| dc.identifier.doi | 10.1127/ejm/5/3/0493 | |
| dc.identifier.wos | A1993LE86800009 | |