Diverse dynamics of Holocene mafic-intermediate Plinian eruptions at Mt. Taranaki (Egmont), New Zealand
Author:
Funder
NZ Natural Hazards Research Platform
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
http://link.springer.com/article/10.1007/s00445-017-1162-4/fulltext.html
Reference94 articles.
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2. Alloway B, Neall VE, Vucetich CG (1995) Late Quaternary (post 28,000 years B.P.) tephrostratigraphy of northeast and central Taranaki, New Zealand. J Royal Soc NZ 25:385–458
3. Andronico D, Cioni R (2002) Contrasting styles of Mount Vesuvius activity in the period between the Avellino and Pompeii Plinian eruptions, and some implications for assessment of future hazards. Bull Volcanol 64(6):372–391
4. Arce JL, Cervantes KE, Macías JL, Mora JC (2005) The 12.1 ka Middle Toluca Pumice: A dacitic Plinian–subplinian eruption of Nevado de Toluca in Central Mexico. J Volcanol Geotherm Res 147:125–143
5. Arce JL, Macías JL, Gardner JE, Rangel E (2012) Reconstruction of the Sibinal Pumice, an andesitic Plinian eruption at Tacaná Volcanic Complex, Mexico–Guatemala. J Volcanol Geotherm Res 217:39–55
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