P. Cordier et al., TEM INVESTIGATION OF DISLOCATION MICROSTRUCTURE OF EXPERIMENTALLY DEFORMED SILICATE GARNET, Physics of the earth and planetary interiors, 97(1-4), 1996, pp. 121-131
Deformation experiments have been carried out on single crystals of ga
rnet (Py25 Al67 Sp2 Gr6) under high confining pressure (P = 6.5 GPa) a
nd temperature (T = 1440 degrees C) in a multi-anvil apparatus. The hi
gh pressure sample assembly was designed so as to generate high differ
ential stress. In one experiment, the differential stress was limited
by a single crystal of San Carlos olivine (oriented along [010]) added
on top of the specimen. Garnet crystals have been plastically deforme
d which shows that under our experimental conditions, garnet is ductil
e. The dislocation microstructure, analysed by transmission electron m
icroscopy (TEM), suggests that both 1/2[111]{110} and [100]{110} glide
systems have been activated. Some dislocations appear to be dissociat
ed. The observations of dislocation junctions and subgrain structures
indicate that dislocation climb is enhanced under our experimental con
ditions.