“…The ra tios be tween rel a tively im mo bile trace el e ments, includ ing La/Sc, Th/Sc, Th/Co and Th/Cr, are also con sid ered suitable in di ca tors of par ent rock prov e nance (e.g., Wron kiewicz and Condie, 1990;Cox et al, 1995;Cullers, 1995;Cai et al, 2011;Ali et al, 2014). This is sup ported by the fact that La, Th and Hf are en riched in fel sic rocks, whereas Co, Cr, and Sc are more concen trated in mafic rocks.…”