M
Mike Burton
Researcher at University of Manchester
Publications - 183
Citations - 7420
Mike Burton is an academic researcher from University of Manchester. The author has contributed to research in topics: Volcano & Magma. The author has an hindex of 43, co-authored 166 publications receiving 6499 citations. Previous affiliations of Mike Burton include Centre national de la recherche scientifique & University of Cambridge.
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Deep Carbon Emissions from Volcanoes
TL;DR: The role of CO2 degassing from the Earth is clearly fundamental to the stability of the climate, and therefore to life on Earth as discussed by the authors, but the uncertainty in our knowledge of this critical input into the geological carbon cycle led Berner and Lagasa (1989) to state that it is the most vexing problem facing us in understanding that cycle.
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A multi-disciplinary study of the 2002-03 Etna eruption: insights into a complex plumbing system
Daniele Andronico,Stefano Branca,Sonia Calvari,Mike Burton,Tommaso Caltabiano,Rosa Anna Corsaro,Paola Del Carlo,Gaetano Garfì,Luigi Lodato,Lusia Miraglia,Filippo Murè,Marco Neri,Emilio Pecora,Massimo Pompilio,G. Salerno,Letizia Spampinato +15 more
TL;DR: The 2002-03 Mt Etna flank eruption began on 26 October 2002 and finished on 28 January 2003, after three months of continuous explosive activity and discontinuous lava flow output.
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Magmatic Gas Composition Reveals the Source Depth of Slug-Driven Strombolian Explosive Activity
Mike Burton,Mike Burton,Mike Burton,Patrick Allard,Patrick Allard,Patrick Allard,F. Murè,F. Murè,F. Murè,Alessandro La Spina,Alessandro La Spina,Alessandro La Spina +11 more
TL;DR: Spectroscopic measurements performed during both quiescent degassing and explosions on Stromboli volcano are used to demonstrate that gas slugs originate from as deep as the volcano-crust interface (∼3 kilometers), where both structural discontinuities and differential bubble-rise speed can promote slug coalescence.
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Spectroscopic evidence for a lava fountain driven by previously accumulated magmatic gas
TL;DR: Analysis of magmatic gas during a powerful lava fountain, measured with Fourier transform infrared spectroscopy on Mount Etna, Sicily, reveals a fountain gas having higher CO2/S and S/Cl ratios than other etnean emissions, and which cannot derive from syn-eruptive bulk degassing of Etna basalt.
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Gradual caldera collapse at Bárdarbunga volcano, Iceland, regulated by lateral magma outflow
Magnús T. Gudmundsson,Kristín Jónsdóttir,Andrew Hooper,Eoghan P. Holohan,Sæmundur A. Halldórsson,Benedikt G. Ófeigsson,Simone Cesca,Kristín Vogfjörd,Freysteinn Sigmundsson,Thórdís Högnadóttir,Páll Einarsson,Olgeir Sigmarsson,Olgeir Sigmarsson,Alexander H. Jarosch,Kristján Jónasson,Eyjólfur Magnússon,Sigrún Hreinsdóttir,Marco Bagnardi,Michelle Parks,Vala Hjörleifsdóttir,Finnur Pálsson,Thomas R. Walter,Martin P. J. Schöpfer,Sebastian Heimann,Hannah I. Reynolds,Stéphanie Dumont,Eniko Bali,Gudmundur H. Gudfinnsson,Torsten Dahm,Matthew J. Roberts,Martin Hensch,Joaquín M. C. Belart,Karsten Spaans,Sigurdur Jakobsson,Gunnar B. Gudmundsson,Hildur M. Fridriksdottir,Hildur M. Fridriksdottir,Vincent Drouin,Tobias Dürig,Guðfinna Aðalgeirsdóttir,Morten S. Riishuus,Gro Pedersen,Tayo van Boeckel,Björn Oddsson,Melissa Anne Pfeffer,Sara Barsotti,Baldur Bergsson,Amy Donovan,Mike Burton,Alessandro Aiuppa +49 more
TL;DR: It is concluded that interaction between the pressure exerted by the subsiding reservoir roof and the physical properties of the subsurface flow path explain the gradual near-exponential decline of both the collapse rate and the intensity of the 180-day-long eruption of the Bárdarbunga volcano.