Abstract
New K‐Ar age determinations indicate that the exposed portion of the Tongariro volcanic complex has grown steadily since at least 275 ka, with intervals of vigorous cone growth at 210–200, 130–70, and 25 ka to the present day.
Keywords:
New Zealand Journal of Geology and Geophysics
Volume 39, 1996 - Issue 1
![Sample our Earth Sciences journals, sign in here to start your access, latest two full volumes FREE to you for 14 days]({"type":"image" , "src" : "/sda/5930/TOC-Subject-Sample-2021-Earth-Sciences.jpg"})
Reprints and Corporate Permissions
Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?
To request a reprint or corporate permissions for this article, please click on the relevant link below:
Academic Permissions
Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?
Obtain permissions instantly via Rightslink by clicking on the button below:
If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.
Related Research Data
Monogenetic volcanism: personal views and discussion
Source:
Springer Science and Business Media LLC
Reconstructing the largest explosive eruptions of Mt. Ruapehu, New Zealand: lithostratigraphic tools to understand subplinian–plinian eruptions at andesitic volcanoes
Source:
Springer Science and Business Media LLC
Subcommission on geochronology: Convention on the use of decay constants in geo- and cosmochronology
Source:
Elsevier BV
Tephrostratigraphy and chronology of late quaternary eruptives from the Tongariro Volcanic Centre, New Zealand
Source:
Informa UK Limited
InSAR observations over the Taupō Volcanic Zone's cone volcanoes: insights and challenges from the New Zealand volcano supersite
Source:
Informa UK Limited
The prevalence of plagioclase antecrysts and xenocrysts in andesite magma, exemplified by lavas of the Tongariro volcanic complex, New Zealand
Source:
Springer Science and Business Media LLC
ERUPTION RATES AND MAGMA BUDGETS
Source:
American Geophysical Union (AGU)
Crustal extension in the Tongariro graben, New Zealand: Insights into volcano-tectonic interactions and active deformation in a young continental rift
Source:
Geological Society of America
Potassium-argon geochronology of a basalt-andesite-dacite arc system: The Mount Adams volcanic field, Cascade Range of southern Washington
Source:
Geological Society of America
Heterogeneous andesite–dacite ejecta in 26–16.6 ka pyroclastic deposits of Tongariro Volcano, New Zealand: the product of multiple magma-mixing events
Source:
Springer Science and Business Media LLC
Palaeomagnetic refinement of the eruption ages of Holocene lava flows, and implications for the eruptive history of the Tongariro Volcanic Centre, New Zealand
Source:
Oxford University Press (OUP)
Lithium metaborate flux in silicate analysis
Source:
Elsevier BV
Small and short-lived magma batches at composite volcanoes: time windows at Tongariro volcano, New Zealand
Source:
Geological Society of London
Linking provided by
