Abstract
Self-consistent mean-field calculations have been performed on nuclei with Z=36, 38. When compared to experimental values, the two neutron separation enegies and the mean-square-charge radii differences are in excellent agreement for isotopes with N>50, providing additional evidence for a region of strong deformation around (Z, N)=(40, 60). For isotopes with N<50 the discrepancy between experiment and calculation can account for large zero-point quadrupole vibrations.