Debris flow evolution and the activation of an explosive hydrothermal system; Te Maari, Tongariro, New Zealand-Reference-Cited by-同舟云学术

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Debris flow evolution and the activation of an explosive hydrothermal system; Te Maari, Tongariro, New Zealand

Published:2014-10 Issue: Volume:286 Page:303-316
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Procter J.N.,Cronin S.J.,Zernack A.V.,Lube G.,Stewart R.B.,Nemeth K.,Keys H.

Funder

New Zealand Natural Hazards Platform

Department of Conservation

Genesis Energy

New Zealand Forest Managers Ltd

Waikato Regional Council

New Zealand Transport Agency

Taupo District Council

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference73 articles.

1. Estimating discharge from superelevation in bends: American Society of Civil Engineers;Apmann;J. Hydraul. Div.,1973

2. A review on phreatic eruptions and their precursors;Barberi;J. Volcanol. Geotherm. Res.,1992

3. Using the spatial distribution and lithology of ballistic blocks to interpret eruption sequence and dynamics: August 6 2012 Upper Te Maari eruption, New Zealand;Breard;J. Volcanol. Geotherm. Res.,2014

4. Characteristics of hydrothermal eruptions, with examples from New Zealand and elsewhere;Browne;Earth Sci. Rev.,2001

5. Textural analysis of particles from El Zaguán debris avalanche deposit, Nevado de Toluca volcano, Mexico: evidence of flow behavior during emplacement;Caballero;J. Volcanol. Geotherm. Res.,2011

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