Winged porphyroclasts are often used as kinematic or strain indicators
in shear zones. In particular, it has been suggested that the geometr
y of delta-clasts in mylonites can give information about the theologi
cal behaviour of the matrix around the clast (Passchier et al., 1993).
We tested this hypothesis with a numerical finite element simulation
of the flow field of a viscous matrix around a relatively rigid clast.
Power-law viscous flow properties of the matrix with stress-exponents
of 1 (linear viscous), 3 and 5 were tested, as well as three differen
t sets of approximately simple shear boundary conditions, which are re
levant to experimental and/or natural situations, The simulations show
that the flow field is primarily determined by the boundary condition
s. The stress-exponent is of secondary importance. In general, the dif
ferent boundary conditions produce two types of flow fields about the
rigid clast: an eye-shaped flow field and a bow-tie shaped flow field.
The former is produced by boundary conditions that approximate simple
shear applied at an infinite distance from the rigid clast, and the l
atter is produced by boundary conditions which are equivalent to a she
ar box or ring shear apparatus. Although both the shear-box and ring-s
hear boundary conditions produce bow-tie flow patterns, the wing geome
tries which result from the flow patterns for these two cases can be s
ignificantly different. The geometry of the wings that develop on a de
lta-clast is a direct function of the flow field around the clast. For
linear and non-linear theologies, only the ring-shear boundary condit
ions produce wings that show ''stair-stepping'' (i.e. wings that are p
arallel but not in the same plane). In natural shear zones, delta-clas
ts both with and without stair-stepping are observed. In comparing geo
logic observations with experimental or numerical modelling, it is ess
ential to understand which boundary conditions are appropriate.