R. Christoffersen et Ak. Kronenberg, DISLOCATION INTERACTIONS IN EXPERIMENTALLY DEFORMED BIOTITE, Journal of structural geology, 15(9-10), 1993, pp. 1077-1095
Biotite single crystals shortened experimentally in orientations that
maximize critical resolved shear stresses on (001) in directions [110]
, [010] and [310] have been examined by transmission electron microsco
py. In all samples, dislocations are confined to the basal plane with
Burgers vectors of 1/2[110] and [100], consistent with previous determ
inations of mica slip systems. Occasional partial dislocations that bo
und stacking faults form extended dislocations of these same systems.
Typically dislocations are concentrated in complex affays in local reg
ions of the samples; isolated or widely spaced dislocations are the ex
ception. Within these arrays, a variety of interactions between the di
slocations are suggested by the geometrical arrangements of dislocatio
ns that cross over one another on parallel (001) planes sufficiently c
lose together for elastic interaction, and dislocations on the same (0
01) plane in networks and parallel arrays. Crossing dislocations of op
posite sign on separate (001) planes form stable dipole segments where
they overlap. Attractive and repulsive interactions between overlappi
ng dislocations of like sign are evident as well. Dislocation networks
occur in all samples and may exhibit a variety of complexly distorted
geometries. The spacing of dislocations in parallel arrays do not mat
ch models for standard dislocation pile-ups, consistent with observati
ons showing thcse arrays involve dislocation multipoles. The observed
dislocation arrays and interactions resemble those reported for Stage
I easy-glide deformation of FCC and HCP metals. Basal shear strengths
are probably largely controlled by the development of multipoles and d
islocations that pile up behind them.