The crystal structure of a rubidian cesian phlogopite-1M from pegmatite exo
contacts at Red Cross Lake, Manitoba, monoclinic, a = 5.343(1), b = 9.247(2
), c = 10.397(3) Angstrom, beta = 100.04(2)degrees, V = 505.8(2) Angstrom(3
), has been refined to an R index of 4.5% based on 519 observed reflections
measured with graphite-monochromated MoKa X-radiation on an automated four
-circle diffractometer. The crystal used in the collection of the X-ray int
ensity data was also analyzed by electron microprobe, giving the unit formu
la (K0.46Rb0.28Cs0.23)(Mg1.20Fe1.0Al0.38Li0.34Mn0.04Ti0.04)(Si2.91Al1.09)O-
10[(OH)(1.55)F-0.45]. The interlayer sire, X, contains large amounts of Rb
and Cs, and cell dimensions and the <X-O> distance are in accord with data
from synthetic Rb and Cs phlogopites and plutonic phlogopites. The interlay
er coordination is much more regular in rubidian cesian phologopite than in
other trioctahedral micas, defining a trend of increasing regularity with
increasing interlayer-cation size.