Earth. Since a major caldera-forming eruption episode at∼ 50 ka,> 50 rhyolitic eruption
episodes have occurred at Okataina Volcanic Centre (OVC) and Taupo Volcanic Centre
(TVC). These two active calderas provide an opportunity to examine contemporaneous
magmatic processes at high temporal and spatial resolution. Temporal trends indicate OVC
intra-caldera eruption episodes tapped progressively more evolved (∼ 71–77 wt.% SiO2) …