TY - JOUR
T1 - The crystal structure of a K-poor Ca-rich silicate with the nepheline framework, and crystal-chemical relationships in the compositional space (K,Na,Ca,□)8(Al,Si)16O32
AU - Rossi, G.
AU - Oberti, R.
AU - Smith, D. C.
PY - 1989
Y1 - 1989
N2 - The crystal structure of a K-poor Ca-rich tectosilicate (a = b = 9.982, c = 8.364 Å, space group P63) with composition close to Ca1□1Na6Al8Si8O32 has been refined using 364 independent reflections collected by a single-crystal X-ray diffractometer. The anisotropic refinement yielded a final R factor equal to 0.037 for the observed reflections. The tetrahedral framework is the same as that of nepheline, but the distribution of the Ca, Na, and K cations is quite unusual: the large A cavity is here statistically occupied by (Ca + Na + K + □), with one position at the K position of ordinary nephelines but occupied by (C+Na+minor K+□), and a second position labelled Ca' and occupied by (Ca+Na+□) displaced along the z axis at approximately 1.25 Å from the K position. A review of the crystal structures in the compositional space (K,Na,Ca,□)8(Al,Si)16O32, which includes kalsilite, nepheline, lisetite, anorthite, tridymite and many polymorphs thereof, is also presented. This reveals that compositions close to the K2Na6-, Na2Na6-, Na2Na6- and Ca1□1Na6- end-members distinguish themselves by having respectively "centred', "off-centred' and "displaced' cations in the large cation site. -Authors
AB - The crystal structure of a K-poor Ca-rich tectosilicate (a = b = 9.982, c = 8.364 Å, space group P63) with composition close to Ca1□1Na6Al8Si8O32 has been refined using 364 independent reflections collected by a single-crystal X-ray diffractometer. The anisotropic refinement yielded a final R factor equal to 0.037 for the observed reflections. The tetrahedral framework is the same as that of nepheline, but the distribution of the Ca, Na, and K cations is quite unusual: the large A cavity is here statistically occupied by (Ca + Na + K + □), with one position at the K position of ordinary nephelines but occupied by (C+Na+minor K+□), and a second position labelled Ca' and occupied by (Ca+Na+□) displaced along the z axis at approximately 1.25 Å from the K position. A review of the crystal structures in the compositional space (K,Na,Ca,□)8(Al,Si)16O32, which includes kalsilite, nepheline, lisetite, anorthite, tridymite and many polymorphs thereof, is also presented. This reveals that compositions close to the K2Na6-, Na2Na6-, Na2Na6- and Ca1□1Na6- end-members distinguish themselves by having respectively "centred', "off-centred' and "displaced' cations in the large cation site. -Authors
UR - http://www.scopus.com/inward/record.url?scp=0024486521&partnerID=8YFLogxK
U2 - 10.1127/ejm/01/1/0059
DO - 10.1127/ejm/01/1/0059
M3 - Article
AN - SCOPUS:0024486521
SN - 0935-1221
VL - 1
SP - 59
EP - 70
JO - European Journal of Mineralogy
JF - European Journal of Mineralogy
IS - 1
ER -