Pure delafossite AgFeO2 prepared by co-precipitation method.
57Fe Mössbauer spectroscopy studies performed at room and low temperatures.
Structural polytypes rhombohedral and hexagonal recognized by X-ray diffraction.
Transition from paramagnetic to magnetic ordering seen by Mössbauer spectroscopy.
Decrease of average hyperfine magnetic field observed with increase of temperature.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址:北京市海淀区学院路29号 邮编:100083 电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700 |