Gadolinium silicate films on Si(100) annealed in oxygen and vacuum at tempe
ratures up to 800 degreesC were analyzed by Rutherford backscattering and n
arrow resonance nuclear profiling. Oxygen diffused into the film eliminatin
g oxygen vacancies, but Si diffusion, previously observed in Al and Y oxide
s and in La and Zr silicate films, was absent. Higher-temperature annealing
in oxygen resulted in the formation of an interfacial layer observable in
high-resolution electron micrographs. Gd0.23Si0.14O0.63 films crystallize a
t temperatures between 1000 and 1050 degreesC. These observations combined
with recent electrical measurements show that gadolinium silicate films may
be a good candidate for the replacement of SiO2 in deep submicron metal-ox
ide-semiconductor gates.