Crystallisation ages in coeval silicic magma bodies: 238U–230Th disequilibrium evidence from the Rotoiti and Earthquake Flat eruption deposits, Taupo Volcanic Zone, New Zealand
- 1 February 2003
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 206 (3-4) , 441-457
- https://doi.org/10.1016/s0012-821x(02)01109-3
Abstract
No abstract availableKeywords
This publication has 37 references indexed in Scilit:
- The 26.5 ka Oruanui eruption, New Zealand: an introduction and overviewJournal of Volcanology and Geothermal Research, 2001
- Stratigraphy and dispersal of the Mangaone Subgroup pyroclastic deposits, Okataina Volcanic Centre, New ZealandJournal of Volcanology and Geothermal Research, 2000
- Late Quaternary evolution of a hyperactive rhyolite magmatic system: Taupo volcanic centre, New ZealandJournal of the Geological Society, 2000
- Volcanic and structural evolution of Taupo Volcanic Zone, New Zealand: a reviewJournal of Volcanology and Geothermal Research, 1995
- An outline geochemistry of rhyolite eruptives from Taupo volcanic centre, New ZealandJournal of Volcanology and Geothermal Research, 1995
- Stratigraphy, chronology, styles and dynamics of late Quaternary eruptions from Taupo volcano, New ZealandPhilosophical Transactions A, 1993
- The Generation of Granitic Magmas by Intrusion of Basalt into Continental CrustJournal of Petrology, 1988
- Ash-flow magmatismPublished by Geological Society of America ,1979
- Late pleistocene tephrostratigraphy in the Taupo district, New ZealandNew Zealand Journal of Geology and Geophysics, 1976
- Rotoehu ash and the Rotoiti Breccia Formation, Taupo Volcanic zone, New ZealandNew Zealand Journal of Geology and Geophysics, 1972