Abstract
The infrared-active lattice vibrations of the orthorombic marcasite (FeS2) have been studied by measuring the reflectivity of different crystal faces at near-normal incidence. A group-theoretical analysis predicts seven infrared-active modes (k = 0). Cartesian symmetry coordinates as well as vibrational modes of the lattice vibrations are constructed

This publication has 0 references indexed in Scilit: