Abstract
Mössbauer and other studies establish that in (), ferromagnetic -rich clusters coexist with paramagnetic -rich regions in the same crystallographic phase, with the ferromagnetic component increasing with increasing and decreasing . The holes created by substitution are itinerant both above and below . All the experimental observations on this system can be explained on the basis of itinerant-electron ferromagnetism.
- Received 25 June 1974
DOI:https://doi.org/10.1103/PhysRevB.12.2832
©1975 American Physical Society