T. Masuda et al., SHAPE PREFERRED ORIENTATION OF RIGID PARTICLES IN A VISCOUS MATRIX - REEVALUATION TO DETERMINE KINEMATIC PARAMETERS OF DUCTILE DEFORMATION, Journal of structural geology, 17(1), 1995, pp. 115-129
The development of the shape preferred orientation of rigid elliptical
bodies during non-coaxial deformation is theoretically simulated in a
two-dimensional Newtonian matrix. The angular velocity of a rigid ell
iptical body (phi) can be expressed as phi = V/R(2) + 1[R(2) sin(2) ph
i cos Theta + Cos(2) phi Cos Theta - (R(2) - 1) sin(2) phi sin Theta]
where phi is the angle between the shear plane and the longest axis of
the ellipse, R is the aspect ratio of the ellipse, V is a constant, a
nd Theta is the newly introduced index angle to describe degree of non
-coaxiality between simple shear and pure shear defined as tan Theta =
epsilon/gamma. gamma and epsilon are simple shear strain rate and pur
e shear strain rate, respectively. The initial distribution pattern of
the elliptical bodies is assumed to be random in an R/phi diagram, ac
id a series of the distribution patterns was calculated using the abov
e equation with increasing deformation at varying Theta. When deformat
ion is simple shear (i.e. Theta = 0 degrees), all elliptical bodies ro
tate with various angular velocities, resulting in a skewed distributi
on in the R/phi diagram. In contrast, for pure shear (i.e. Theta = 90
degrees) all of them asymptotically settle their longest axes on a pla
ne perpendicular to the compression axis, resulting in strongly concen
trated and symmetric distribution patterns in the R/phi diagram. When
deformation is general noncoaxial (0 degrees < Theta < 90 degrees), di
stribution patterns in the R/phi diagram change systematically from th
e pattern similar to that of Theta = 0 degrees to that of Theta = 90 d
egrees with increasing Theta. These R/phi diagrams can be used for est
imating the degree of non-coaxiality. We analyzed shape preferred orie
ntation of porphyroclasts in two mylonites, and concluded that deforma
tion within the mylonites contain a certain amount of pure shear compo
nent that superimposes on a simple shear component.