A very efficient energy transfer from Fe3+ (d tetrahedral sites) to Tm
3+ (c dodecahedral sites) in yttrium aluminum garnet and gadolinium ga
llium garnet crystals was observed. The site-selective spectroscopy sh
ows that in case of near-neighbor Fe(d)-Tm pairs the transfer efficien
cy is 100%. For the other pairs it is less efficient and increases wit
h temperature due to a better superposition of Fe3+ emission and H-3(4
) Tm3+ absorption bands.