“…The residues after high degrees of melting are commonly highly depleted in incompatible elements, compared to the low-degree melting residues, in both bulk and mineral chemistry. Aktimur et al, 1995;Özen et al, 2008;Sarifakioglu et al, 2009), showing the peridotite sample locations. Inset map displays the major tectonic belts (Dinter, 1998) and the distribution of major ophiolite complexes in Turkey (Dilek and Furnes, 2009).…”