Fig. 5From: Evolution of the Earth as an andesite planet: water, plate tectonics, and delamination of anti-continentMineral assemblages in the sub-IBM arc crust and mantle along a possible geotherm for the inferred crust and mantle components listed in Table 1 for different basalt-rhyolite mixtures. Compared to the model in Tatsumi et al. (2008), this model uses a lower temperature to maintain subsolidus temperatures at the MohoBack to article page