Abstract
Experimental evidence from the spectroscopy of155Gd and153Sm for the theoretically predicted quadruplet band structure, with band parity sequences (+−−+) and (−++−), is examined.
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We wish to thank Dr. R. Piepenbring for illuminating discussions on the differences between octupole correlations in the actinides and in the rare earths. These investigations were supported by the National Science Foundation under contract number PHYS9-06613 with the Florida State University.
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Sheline, R.K., Sood, P.C. Quadruplet spectroscopy in the region of strong nuclear octupole correlations. Czech J Phys 40, 622–628 (1990). https://doi.org/10.1007/BF01597858
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DOI: https://doi.org/10.1007/BF01597858