Yp. Li et al., The crystal structure of thornasite, Na12Th3[Si8O19](4)(H2O)(18): A novel interrupted silicate framework, AM MINERAL, 85(10), 2000, pp. 1521-1525
The crystal structure of thornasite, Na12Th3[Si8O19](4)(H2O)(18), Z = 6, rh
ombohedral, a = 29.124(1), c = 17.2602(9) Angstrom, V = 12,679.2(9) Angstro
m(3), space group R (3) over bar c, has been solved by direct methods, and
refined to an agreement index (R1) of 5.7% calculated, based on 2266 unique
observed reflections collected using MoK alpha X-radiation and a CCD-based
detector. The structure consists of a new interrupted silicate framework w
ith composition [Si8O19](6-). The framework density is 15.4 atoms per 1000
Angstrom(3), which is typical for microporous aluminosilicate materials. Th
e framework density, together with the presence of a three-dimensional netw
ork of channels in the structure, permit thomasite to be designated as a ne
w member of the zeolite structure family. The framework consists of cubic c
ages and distorted six-membered rings linked via common edges. The circuit
symbol is (4(3)14(3))(4(3)6(2)14)(3)(6.10.12)(3)(6(2)10)(6). Interruptions
of the framework are caused by the presence of Th4+ cations that are coordi
nated by eight O atoms. Na+ cations and H2O groups are located in channels
through the structure. The theoretical parent framework for thornasite may
be constructed by the insertion of two additional Si atoms in place of one
Th atom. The theoretical framework density is 18.0 atoms per 1000 Angstrom(
3); the circuit symbol is (4(3)10(3))(4(3)6(2)10)(6)(4(3)6(2)8)(3)(4(3)6.8.
10)(3)(4(2)6(2)8.10)(3)(4(1)6(3)8.10)(3).