Abstract
A shell-model description of the structure of low-energy states of heavy deformed nuclei is used to predict the number and strengths of 1 + states that couple to the ground state via a strong M1 transition. Results are given for the magnetic moments of 2 g + states of various Gd, Er, U, and Pu isotopes and also the M1 transition strengths 1 + → 0 g +, 1 + → 2 g +, and 1 + → 2 γ + for several rare earth and actinide nuclei.
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