摘要
A [3Fe-3(mu-S)](3+) cluster is reported in which each ferric center has a distorted trigonal pyramidal geometry, with an S = 1/2 ground state for the cluster and unusually anisotropic hyperfine coupling constants as determined by variable temperature magnetometry and Mossbauer spectroscopy.
- 出版日期2016
- 单位中国地震局; 西北大学