It is shown in this letter that, in contrast to the accepted belief in the
literature, it is possible to determine if a minority component is located
on the dodecahedral, octahedral, or tetrahedral sites in a garnet single cr
ystal. This prediction of ours is based on dynamical Bloch-wave calculation
s and proved experimentally with x-ray measurements in a transmission elect
ron microscope. The previous literature seemed to agree on the assumption t
hat the dodecahedral and tetrahedral sites are indistinguishable from each
other. (C) 1999 American Institute of Physics. [S0003-6951(99)04125-X].