“…The skarn zonation is controlled by temperature, depth of formation, fluid/rock ratios, compositions and oxidation state of associated intrusions and wall rocks (Chowdhury and Lentz, 2011;Deng et al, 2011Deng et al, , 2014cFuertes-Fuente et al, 2000;Kuşcu et al, 2002;Levresse and Gonzalez-Partida, 2003;Meinert et al, 2005;Oyman, 2010;Pons et al, 2010;Scheepers, 2000;Somarin and Moayyed, 2002; Williams-Jones -2 2 1 1 1 3 1 1 1 2 1 1 2 6 1 7 3 3 1 1 II I I I II II II II II II II III III III III III , 2010). The garnet/clinopyroxene ratios can give important clues about these fundamental geological variables, serve as a crude indicator of the general oxidation state of the system, and be applied to both the classification and exploration of the skarn deposits (Einaudi, 1981;Gaspar et al, 2008;Logan, 2000;Lu et al, 2003;Meinert et al, 1997b;Öztürk and Helvaci, 2008;Somarin, 2004).…”