Hw. Xu et Pj. Heaney, MEMORY EFFECTS OF DOMAIN-STRUCTURES DURING DISPLACIVE PHASE-TRANSITIONS - A HIGH-TEMPERATURE TEM STUDY OF QUARTZ AND ANORTHITE, The American mineralogist, 82(1-2), 1997, pp. 99-108
Memory effects associated with the Dauphine twins in alpha quartz and
the c-antiphase domains (c-APDs) in P (1) over bar anorthite have been
investigated by in situ hot-stage transmission electron microscopy (T
EM). In a set of kinetic experiments, specimens were cycled about thei
r transition temperatures, and changes in the Dauphine twin and c-APD
positions were analyzed as a function of maximum annealing temperature
and annealing time. The results indicate that Dauphine twins are stro
ngly pinned by extended defects, such as Brazil twin and grain boundar
ies, dislocations, and surfaces. However, the memory displayed by Daup
hine twin boundaries pinned by point defects degrades with higher anne
aling temperatures and longer annealing times. An Arrhenius analysis o
f this behavior yielded an average activation energy for point-defect
diffusion of 68.6 kJ/mol. In contrast to the Dauphine twins of quartz,
the c-APDs of anorthite did not appear to interact strongly with exte
nded defects, and they exhibited a nearly perfect memory for all annea
ling times and temperatures tested. This extremely high fidelity is in
terpreted as evidence that the positions of c-APDs are fixed by locali
zed Al-Si disorder, which remains unchanged when anorthite is heat tre
ated at <1000 degrees C.