Article ID Journal Published Year Pages File Type
10709825 Journal of Magnetism and Magnetic Materials 2012 8 Pages PDF
Abstract
► Inverse TMR in the Ag buffered MTJ is due to Fe3O4 formed at CoFe/AlOx interfaces. ► STEM EELS SIs provide the evidences for formation of Fe3O4. ► High oxygen solubility in Ag can be the reason for the formation of Fe3O4.
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Related Topics
Physical Sciences and Engineering Physics and Astronomy Condensed Matter Physics
Preview
Inverse TMR in a nominally symmetric CoFe/AlOx/CoFe junction induced by interfacial Fe3O4 investigated by STEM-EELS
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