Stuchbery, A. E.White, A. G.Dracoulis, G. D.Schiffer, K. JFabricius, B.2025-12-312025-12-310939-7922ORCID:/0000-0002-0198-9901/work/165830272https://hdl.handle.net/1885/733798083Transient-field precessions were measured simultaneously for levels in the ground-state bands of156, 158, 160Gd as ions of these nuclei traversed a thin polarized Fe foil. Relative g-factors of levels up to 61+ were deduced, those of the 41+ levels being determined with greatest precision. In contrast with the conclusions of the recent report by Alzner et al. [1], our results are consistent with g(41+) having the same value in all three isotopes and imply g(21+)=g(41+) in156Gd, consistent with nuclear structure models.4en21.10.Ky27.70+ q199110.1007/BF012847860000093353