The crystal structure of parisite-(Ce) was solved and refined to R = 0.044,
Rw = 0.037 using three-dimensional X-ray diffraction data (XRD). In contra
st to the putative hexagonal cell, weak XRD maxima on precession films demo
nstrate that the parisite-(Ce) is monoclinic with a space group C2/c Or CC.
The unit cell was refined as a = 12.305(2), b = 7.1053(5), c = 28.250(5) An
gstrom, and beta = 98.257(14)degrees The structure refinement confirmed the
space group Cc. Like bastnasite and synchysite, parisite possesses a (001)
layer structure, with layers of (Ca) and (CeF) separated by layers of carb
onate groups. The [001] layer stacking sequence is... (Ca), (CO3), (CeF), (
CO3), (CeF), (CO3), (Ca), (CO3), (CeF), (CO3), (CeF), (CO3)....
The parisite-(Ce) structure can be considered as two portions of the bastna
site structure connected by a (Ca) layer. The insertion of a (Ca) layer wou
ld create long [001]*: structure voids in the F columns if the bastnasite p
ortions stacked hexagonally; therefore, the two bastnasite portions are off
set along [(1) over bar 10] by a/6(sin60 degrees) (or [(1) over bar 00] in
hexagonal cells, by a/3) such that the oxygen atoms of the vertical edges o
f the carbonate groups occupy the voids. Polytypism results because a bastn
asite portion can shift equally in two possible directions, +/-120 degrees
from the previous offset vector. The parisite-(Ce) structure elucidated her
ein is the simplest and most common polytype possible. 2M. The polytype 6R,
which was previously believed to be the most common, has not been found du
ring our extensive study.