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The Valles Caldera complex in north–central New Mexico, USA, represents the type example of a resurgent caldera system, characterized by eruption of two voluminous high-silica rhyolite ignimbrites, the Otowi and Tshirege Members of the Bandelier Tuff. Central resurgence of ∼1000 m occurred within 27 ± 27 kyr following eruption of the Tshirege, or Upper Bandelier Tuff (UBT). This process was accomp...

journal of petrology

Magmatic Recharge during the Formation and Resurgence of the Valles Caldera, New Mexico, USA: Evidence from Quartz Compositional Zoning and Geothermometry