Paleomagnetic determination of the age and properties of the 1780–1800 AD dome effusion/collapse episode of Mt. Taranaki, New Zealand
Author:
Funder
AINSE
George Mason Charitable Trust
Natural Hazards Research Platform
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
http://link.springer.com/content/pdf/10.1007/s00445-019-1275-z.pdf
Reference75 articles.
1. Alloway BV, Neall VE, Vucetich CG (1995) Late Quaternary (post 28,000 year B.P.) tephrostratigraphy of northeast and central Taranaki, New Zealand. J Roy Soc NZ 25:385–458. https://doi.org/10.1080/03014223.1995.9517496
2. Andreastuti S, Paripurno E, Gunawan H, Budianto A, Syahbana D, Pallister J (2017) Character of community response to volcanic crises at Sinabung and Kelud volcanoes. J Volcanol Geotherm Res. https://doi.org/10.1016/j.jvolgeores.2017.01.022
3. Aramaki S, Akimoto S-i (1957) Temperature estimation of pyroclastic deposits by natural remanent magnetism. Am J Sci 255:619–627
4. Bardot L, McClelland E (2000) The reliability of emplacement temperature estimates using paleomagnetic methods: a case study from Santorini, Greece. Geophys J Int 143:39–51. https://doi.org/10.1046/j.1365-246x.2000.00186.x
5. Blake S (1990) Viscoplastic models of lava domes. In: Fink JH (ed) Lava flows and domes. IAVCEI Proceedings In Volcanology, vol 2. Springer, Berlin, Heidelberg
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