The one-dimensional model to analyse the kinematics of crystallographic pre
ferred orientation of Ribe (1989) is presented and developed further. It is
argued that this approach can be applied to rotational deformations where
the predominant deformation mechanism is grain boundary sliding. Two contra
sting situations are distinguished. The first is where lattice rotations of
opposing sense occur and there are orientations for which the rotation rat
e is zero. In this case a continually intensifying preferred orientation at
an orientation with zero rotation rate will result. The second situation i
s where the rotation of the lattice is in the same sense for all orientatio
ns. Initially maxima develop in the orientation of greatest negative diverg
ence in the lattice rotation rate function. A steady-state preferred orient
ation profile is possible which is the normalised inverse of the function d
escribing lattice rotation rate vs. orientation and the maxima are at the o
rientations for which the lattice rotation rate is a minimum. The intensity
of the preferred orientation is a function of the ratio of the greatest to
least lattice rotation rates. The results are applied to a natural mylonit
e preferred orientation which consists of a c axis maximum in the mylonitic
foliation perpendicular to the stretching lineation. It is argued that the
crystal lattices rotate about a stably oriented c axis and the profile thr
ough the orientation distribution describing the probability of finding par
ticular orientations differing by a rotation about c is inverted to give an
estimate of the lattice rotation rate profile. It is found that the lattic
e rotates slowest when the second-order prism direction a is aligned parall
el to the foliation normal and fastest when a is aligned sub-parallel to th
e stretching lineation. (C) 1999 Elsevier Science B.V. All rights reserved.