High field magnetic transitions in the mixed holmium–yttrium iron garnet Ho0.43Y2.57Fe5O12

2004 ◽  
Vol 17 (1) ◽  
pp. 241-248 ◽  
Author(s):  
A Bouguerra ◽  
S Khène ◽  
S de Brion ◽  
G Chouteau ◽  
G Fillion
1983 ◽  
Vol 27 (1) ◽  
pp. 326-333 ◽  
Author(s):  
S. Geller ◽  
G. Balestrino ◽  
A. K. Ray ◽  
A. Tucciarone

2008 ◽  
Vol 20 (29) ◽  
pp. 295231 ◽  
Author(s):  
A Bouguerra ◽  
G Fillion ◽  
S de Brion ◽  
S Khène ◽  
P Wolfers ◽  
...  

1977 ◽  
Vol 23 (9) ◽  
pp. 657-659 ◽  
Author(s):  
R.V. Pisarev ◽  
J. Schoenes ◽  
P. Wachter

Author(s):  
J.Y. Laval

The exsolution of magnetite from a substituted Yttrium Iron Garnet, containing an iron excess may lead to a transitional event. This event is characterized hy the formation of a transitional zone at the center of which the magnetite nucleates (Fig.1). Since there is a contrast between the matrix and these zones and since selected area diffraction does not show any difference between those zones and the matrix in the reciprocal lattice, it is of interest to analyze the structure of the transitional zones.By using simultaneously different techniques in electron microscopy, (oscillating crystal method microdiffraction and X-ray microanalysis)one may resolve the ionic process corresponding to the transitional event and image this event subsequently by high resolution technique.


1997 ◽  
Vol 07 (C1) ◽  
pp. C1-283-C1-286
Author(s):  
P. Novák ◽  
J. Englich ◽  
H. Stepánková ◽  
J. Kohout ◽  
H. Lütgemeier ◽  
...  

1971 ◽  
Vol 32 (C1) ◽  
pp. C1-200-C1-201 ◽  
Author(s):  
P. HANSEN ◽  
W. TOLKSDORF

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