The crystal structure of the mineral merlinoite Na5K7(H2O)(24)[Al12Si20O64]
was established by the method of X-ray diffraction analysis. X-ray data we
re collected on a STOE IPDS diffractometer (lambda MoKalpha radiation, grap
hite monochromator, T= 120 K, 2 theta(max) = 62 degrees, R = 0.0434 based o
n 1471 reflections) from a twinned crystal [the (110) twinning parameter is
0.245]: a = 13.863(3) Angstrom, b = 14.135(2) Angstrom, c = 10.047(2) Angs
trom, sp. gr. D-2h(25) = Immm, Z = 1, p(calcd) = 2.269 g/cm(3). Unlike mine
rals studied earlier, merlinoite, a new rare variety of zeolite, does not c
ontain alkaline-earth cations and is characterized by the maximum number of
atoms occupying interstices of the tetrahedral Si,Al,O-framework. A compar
ative crystallochemical analysis of merlinoites of different compositions h
as been performed.