Fig. S2. Construction of a Paleozoic–Mesozoic accretionary orogen along the active continental margin of SE Gondwana (South Island, New Zealand): summary and overview

Geochemical discrimination plot comparing the composition of the mainly Late Jurassic Park Volcanic Group of the Murihiku Terrane with other potential source compositions (for data sources see Robertson & Palamakumbura 2019<i>a</i>). The plot indicates that the Park Volcanic Group would not be readily recognizable in detrital material, as in the Murihiku Supergroup.