“…In particular, the melting of the late transition metal iron at high pressures has wide scientific implications, including geophysical and geochemical modeling of the Earth's interior. This fact has triggered a substantial effort to determine the melting curve of Fe (for a review see: Boehler, R. et al, 2007) and other transition metals including Mo, Ta, and W (Belonoshko et al, 2008;Cazorla et al, 2008;Dai et al, 2009;Errandonea et al, 2001;Errandonea et al, 2003;Foata-Prestavoine et al, 2007;Hixon et al, 1989;Liu et al, 2008;Moriarty et al, 2002;Santamaría-Pérez et al, 2009;Taioli et al, 2007;Zhang et al, 2009). However, despite important advances in experimental and theoretical methods, considerable controversy exists about the pressure dependence of the melting temperatures ( M T ) of Mo, Ta, and W.…”