Gk. Rozenberg et al., HIGH-PRESSURE METALLIZATION AND ELECTRONIC-MAGNETIC PROPERTIES OF HEXAGONAL CUBANITE (CUFE2S3), Physics and chemistry of minerals, 24(8), 1997, pp. 569-573
Fe-57 Mossbauer studies at room temperature and temperature-dependent
resistance studies have been performed on a natural specimen of cubani
te (CuFe2S3) in a diamond-anvil cell at pressures up to similar to 10
GPa. An insulator-metal phase transition occurs in the range 3.4-5.8 G
Pa coinciding with a previously observed structural transition from an
orthorhombic to a hexagonal NiAs (B8) structure. The room temperature
data shows that the metallization process concurs with a gradual tran
sition from a magnetically ordered phase at low pressure to a nonmagne
tic or paramagnetic phase at high-pressure. The change in magnetic beh
aviour at the structural transition may be attributed to a reduction o
f the Fe-S-Fe superexchange angle formed by edge-sharing octahedra. oc
curring in the high-pressure phase. The non-magnetic or paramagnetic m
etallic phase at high pressure is retained upon decompression to ambie
nt pressure-temperature conditions, indicative of substantial hysteres
is associated with the pressure driven orthorhombic-->hexagonal struct
ural transition. The pressure evolution of both the Fe-57 Mossbauer hy
perfine interaction parameters and resistance behaviour is consistent
with the transition from mixed-valence character in the low pressure o
rthorhombic structure to that of extended-electron delocalization in t
he hexagonal phase at high-pressure.