Oxygen-implanted and annealed GaAs:Si epitaxial layers have been inves
tigated by low-temperature Fourier transform infrared absorption spect
roscopy. Several new local vibrational modes are observed in the range
from 614 to 641 cm(-1). Isotope shifts and splittings allow the unamb
iguous chemical identification of the defect involved as SiO2. A micro
scopic structure model is developed which provides, based upon a simpl
e fit, the correct vibrational frequencies. Evidence is presented that
deep levels associated with this complex are causing the high sheet r
esistance of the layers.