A tectonic model for the juxtaposition of granulite- and amphibolite-facies rocks in the Eburnean orogenic belt (Sassandra-Cavally domain, Côte d’Ivoire)

Open Access

Fig. 9

P–T pseudosections and compositional isopleths calculated for the samples (a) SAN in the model system NCKFMASHTO, and (b) MAD1A in the model system MnNCKFMASHTO. Red arrows show the inferred P–T paths. See text for details.

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