Cutts et al. (2014) combined thermodynamic modeling of compositional change in metamorphic garnet with metamorphic peak and retrograde pressure-temperature (P-T) data derived from quantitative P-T pseudosections to determine clockwise P-T paths for several samples from the Tjakastad schist belt. The Tjakastad schist belt is located in the central portion of the Stolzburg domain1 at the southwestern end of the Barberton Granite-Greenstone Belt (BGGB). The Stolzburg domain is part of the older southern terrane in the BGGB, which lies south of the Saddleback-Inyoka fault system—an inferred suture (de Ronde and de...

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