Griffiths phase in solid-solution of ferromagnetic manganite and cobaltite
arXiv:1109.1090
Abstract
We report the existence of Griffiths phase (GP) over a wide range of in LaSrMnCoO, the solid solution of ferromagnetic (FM) LaSrMnO and LaSrCoO, from magnetization measurements. In this compound, GP arises due to the quenching of randomly distributed Co-O-Mn antiferromagnetic bonds in the FM background. In contrary to divalent doped manganites, GP in the present system can exist entirely in the metallic state above (for 0.10). Based on the present study, a magnetoelectronic phase diagram is drawn.
5 pages, 3 Figures