The mechanism of oxidation-induced stacking fault (OSF) formation in C
zochralski silicon (CZ-Si) crystals was investigated by transmission e
lectron microscopy observations of the initial stages of OSF growth. O
SFs were observed to be always generated at one of the [110] edges of
platelet oxygen precipitates. We observed previously that these platel
et oxygen precipitates had an expansive strain field in the direction
parallel to the precipitate plate and a compressive strain field norma
l to the plate. Silicon self-interstitials having compressive strain a
re probably attracted to the expansive strain field of the precipitate
s, and condense to form stacking faults. A new model for OSF generatio
n is presented taking into consideration the strain field around self-
interstitials and oxygen precipitates.