Fig. 9
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Compositions des cassitérites dans le diagramme ternaire (Sn + Ti + W) − (Mn + Fe) − (Nb + Ta) (% at.). (1) représente la droite de substitution (Fe,Mn)2+ + 2(Nb,Ta)5+ ↔ 3(Sn,Ti)4+ d’après Černý et al. (1985). Les trends magmatique et hydrothermal sont d’après Tindle et Breaks (1998) et Breiter et al. (2007).
Cassiterite compositions plotted in the at. (Sn + Ti + W) − (Mn + Fe) − (Nb + Ta) ternary diagram. (1) represents the (Fe,Mn)2+ + 2(Nb,Ta)5+ ↔ 3(Sn,Ti)4+ substitution line after Černý et al. (1985). Magmatic and hydrothermal trends drawn after Tindle and Breaks (1998) and Breiter et al. (2007).
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