Post-supereruption Magmatic Reconstruction of Taupo Volcano (New Zealand), as Reflected in Zircon Ages and Trace Elements
New zircon U-Th model-age and trace element datasets are presented fromTaupo volcano (New Zealand), which are used to investigate the timescales and broad-scale magmatic processes involving zircon crystallization after the caldera-forming 25·4 ka Oruanui
|Collections||ANU Research Publications|
|Source:||Journal of Petrology|
|01_Barker_Post-supereruption_Magmatic_2014.pdf||2.5 MB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.