IntroductionThe rare earth-transition metal intermetallic compounds are attracting great interest caused not only by their application as materials for permanent magnets but also as opportunities for extended studies of magnetic properties of the 3d and 4f elements.The crystallographic structure of the ternary R-Co-B system, i.e. compounds R,, , C O~~+ , B~, , , was originally investigated by Kuzma and Bilonizhko [l]. Compounds in this series are known to exist for n = 0 (RCo,), n = 1 (RCo,B), n = 2 (R,Co,,B,), n = 3 (R,Co,B,), and n + co (RCo,B,).The Y,Co,,B, borides crystallize in a hexagonal structure of Ce,Co, ,B, type, space group P6/mm [l]. In this structure, rare earth atoms are distributed on two different crystallographic sites (la, 2e), the cobalt atoms on three different positions (2c, 6i,, 6i2), and boron is located on one type of site.The earliest studies of the structural and magnetic properties of R,+ , C O ,~+ 5B2n (R = Sm, Gd) alloys have been carried out Elmasry and Stadelmaier [2] and Smit et al. [3]. Recent Mossbauer studies [3] on the Gd,+ ,Co,,+ ,BZn series have shown that boron increases significantly the rare earth sublattice anisotropy via an enhancement of the second-order crystal field parameter at the R sites. The strength of the individual contributions to the magnetic anisotropy of the non-equivalent cobalt sites in these compounds was thoroughly studied by several researches [4, 51. The compound Sm,Co, ,B,, which corresponds to the case of n = 2 in the above formula, has been reported by Gupta et al. [6], to have a huge anisotropy field of 175 kOe at 295 K.