COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES, cilt.326, sa.11, ss.771-778, 1998 (SCI-Expanded)
Wollastonite-garnet skarns of Demir Tepe (Turkey) are developed in graphitic marbles, forming roof-pendants in the granodioritic Tertiary pluton of Goynukbelen, at the contact of stocks and veins of diorite-monzodiorites that intrude the main pluton. Skarn formation includes several superposed stages