An extended transmission-electron-microscopy investigation of oxygen-i
mplanted silicon has been carried out and has given evidence for a new
precipitation mechanism. This mechanism is related to SiO2 precipitat
ion of free oxygen involved in dense and hot collisional cascades and
produces the largest precipitates in the region where oxygen concentra
tion is still high but primary events originating the collisional casc
ades are no longer sufficient to guarantee the spatial covering of the
silicon. This mechanism prevails at relatively low fluence, while at
high fluence the conventional precipitation dominates; in the present
experimental conditions (energy = 100 keV, target temperature congruen
t-to 250-degrees-C) the oxygen fluence separating these two behaviors
is in the interval 1 X 10(16)-1 X 10(17) cm-2.