Abstract:Exceptionally voluminous arc‐related rhyolitic eruptions from clusters of caldera complexes, as seen in Snowdonia, North Wales (mid‐Caradoc), and North Island, New Zealand (late Neogene‐Quaternary), are characteristically confined within transient, fault‐controlled corridors in continental crust. New Zealand rhyolitic corridors (Coromandel, Central, Taupo) have developed in response to the spearheading of an oceanic arc into continental crust, combined with subduction rollback‐induced extension during clockwis… Show more
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