Abstract
We provide evidence for the existence of a {\em quantum critical point} at the metallization of magnetite FeO at an applied pressure of GPa. We show that the present ac magnetic susceptibility data support earlier resistivity data. The Verwey temperature scales with pressure , with . The resistivity data shows a temperature dependence , with above and 2.5 at the critical pressure, respectively. This difference in with pressure is a sign of critical behavior at . The magnetic susceptibility is smooth near the critical pressure, both at the Verwey transition and near the ferroelectric anomaly. A comparison with the critical behavior observed in the Mott-Hubbard and related systems is made.
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