A statistical model of the bipolar von Mises type was applied to the analys
is of mineral lineation defined by the preferred dimensional orientation of
inequant grains on a foliation surface. Orientation data of 203-258 grains
from each of four rock specimens fit the model well, suggesting a useful a
nalytical technique with three advantages: (1) confidence in whether a meta
morphic tectonite has a mineral lineation can be determined using a chi(2)-
test, (2) the orientation of the mineral lineation can be represented by th
e mean direction (a) with a specified confidence interval, and (3) the degr
ee of preferred dimensional orientation of grains can be quantified by the
concentration parameter (<(kappa)over cap>). (C) 1999 Elsevier Science Ltd.
All rights reserved.