“…Because of this, DAFS may distinguish the valence and local environment of atoms of the same atomic number located on different crystallographic sites. This has been used, for example, to recover the Fe scattering anomalous terms of the tetrahedral and octahedral sites in magnetite [Pickering et al, 1993a], the local environment of Cu1 and Cu2 sites in the superconductor Y Ba 2 Cu 3 O 7 [Cross et al, 1997, Cross et al, 1998b, and the interface structure of an Ir/Fe superlattice [Renevier et al, 1997]. In the special case of magnetite, there exist Bragg reflections strictly sensitive either to the octahedral or tetrahedral sites and without contribution from the other site.…”