|
|
|
|||||||||||||||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |
Universitaet Bremen, Fachbereich Geowissenschaften (Kristallographie), Bremen, Federal Republic of Germany
Johannes-Gutenberg-Universitaet Mainz, Federal Republic of Germany
The crystal structure of a synthetic NaAlSiO 4 modification has been solved and refined to an R index of 0.020 for 2745 independent reflections. The compound is hexagonal with space group symmetry P6 1 , a = 9.995(2) Aa and c = 24.797(4) Aa. The crystal showed twinning by merohedry according to m 210 , which was accounted for in the calculations. The phase was named trinepheline, following prior studies, because the length of its c lattice parameter is three times the length of the c parameter in nepheline, whereas the a parameter is about 10 Aa in both phases. The crystal structure is characterized by layers of six-membered tetrahedral rings of exclusively oval conformation. The rings are built up by regularly alternating AlO 4 and SiO 4 tetrahedra. The stacking of the layers parallel to the c axis results in a three-dimensional network containing channels that are occupied by the Na cations. Although structural similarities with respect to tridymite derivatives can be found, hexagonal trinepheline represents a new type of stuffed tridymite that is not a simple superstructure of nepheline.
This record provided courtesy of AGI/GeoRef.
This article has been cited by other articles:
![]() |
P. Vulic, V. Kahlenberg, and J. Konzett On the existence of a Na-deficient monoclinic trinepheline with composition Na7.85Al7.85Si8.15O32 American Mineralogist, July 1, 2008; 93(7): 1072 - 1079. [Abstract] [Full Text] [PDF] |
||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |