Deep level transient spectroscopy (DLTS) was carried out on single cry
stals of the layered chalcogenide p-GaTe using Schottky barriers paral
lel and perpendicular to the layer planes to study the possible anisot
ropy of the defect levels. Deep levels with the same energies (0.28 eV
and 0.42-0.45 eV) have been found in both directions with concentrati
ons ranging from 10(13)cm(-3) to 10(14)cm(-3) and capture cross-sectio
ns from 10(-15)cm(2) to 10(-17)cm(2). The difference in the spectra ob
tained from the two planes and the possible reason for the deep level
energies being independent of crystal orientation are discussed.