The Whakamaru group ignimbrites, Taupo Volcanic Zone, New Zealand: evidence for reverse tapping of a zoned silicic magmatic system
- 1 August 1998
- journal article
- Published by Elsevier in Journal of Volcanology and Geothermal Research
- Vol. 84 (1-2) , 1-37
- https://doi.org/10.1016/s0377-0273(98)00020-1
Abstract
No abstract availableThis publication has 47 references indexed in Scilit:
- Origin of broken phenocrysts in ash-flow tuffsGSA Bulletin, 1997
- Geochemical zoning and eruptive mixing in ignimbrites from Mangakino volcano, Taupo Volcanic Zone, New ZealandJournal of Volcanology and Geothermal Research, 1993
- Petrology of the zoned calcalkaline magma chamber of Mount Mazama, Crater Lake, OregonContributions to Mineralogy and Petrology, 1989
- The origin of island arc high-alumina basaltsContributions to Mineralogy and Petrology, 1987
- Density and viscosity gradients in zoned magma chambers, and their influence withdrawal dynamicsJournal of Volcanology and Geothermal Research, 1986
- Lead isotope differences between whole-rock and phenocrysts in recent lavas from southern ItalyNature, 1985
- Eruptions from zoned magma chambersJournal of the Geological Society, 1981
- Recognition and correlation of subdivisions within the Whakamaru Ignimbrite, central north island, New ZealandNew Zealand Journal of Geology and Geophysics, 1976
- The iron-titanium oxides of salic volcanic rocks and their associated ferromagnesian silicatesContributions to Mineralogy and Petrology, 1966
- Ash-flow deposits of the central king country, New ZealandNew Zealand Journal of Geology and Geophysics, 1965