Magma generation at a large, hyperactive silicic volcano (Taupo, New Zealand) revealed by U-Th and U-Pb systematics in zircons

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Abstract

Young ( <15 km deep) crust below the volcano. © Oxford University Press, 2004; all rights reserved.

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Charlier, B. L. A., Wilson, C. J. N., Lowenstern, J. B., Blake, S., van Calsteren, P. W., & Davidson, J. P. (2005). Magma generation at a large, hyperactive silicic volcano (Taupo, New Zealand) revealed by U-Th and U-Pb systematics in zircons. Journal of Petrology, 46(1), 3–32. https://doi.org/10.1093/petrology/egh060

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