Unexpected large eruptions from buoyant magma bodies within viscoelastic crust
Large-volume volcanic eruptions can occur despite only limited precursory activity. Here the authors show that modelling the combined effects of buoyant magma, viscoelastic earth behaviour, and sustained magma channels can explain such behaviour of volcanoes and gives an estimate of pressure evoluti...
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Nature Portfolio
2020
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oai:doaj.org-article:0c024d3baeee4898b806085012a75a922021-12-02T15:43:22ZUnexpected large eruptions from buoyant magma bodies within viscoelastic crust10.1038/s41467-020-16054-62041-1723https://doaj.org/article/0c024d3baeee4898b806085012a75a922020-05-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-16054-6https://doaj.org/toc/2041-1723Large-volume volcanic eruptions can occur despite only limited precursory activity. Here the authors show that modelling the combined effects of buoyant magma, viscoelastic earth behaviour, and sustained magma channels can explain such behaviour of volcanoes and gives an estimate of pressure evolution in magma bodies.Freysteinn SigmundssonVirginie PinelRonni GrapenthinAndrew HooperSæmundur A. HalldórssonPáll EinarssonBenedikt G. ÓfeigssonElías R. HeimissonKristín JónsdóttirMagnús T. GudmundssonKristín VogfjördMichelle ParksSiqi LiVincent DrouinHalldór GeirssonStéphanie DumontHildur M. FridriksdottirGunnar B. GudmundssonTim J. WrightTadashi YamasakiNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-11 (2020) |
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Science Q Freysteinn Sigmundsson Virginie Pinel Ronni Grapenthin Andrew Hooper Sæmundur A. Halldórsson Páll Einarsson Benedikt G. Ófeigsson Elías R. Heimisson Kristín Jónsdóttir Magnús T. Gudmundsson Kristín Vogfjörd Michelle Parks Siqi Li Vincent Drouin Halldór Geirsson Stéphanie Dumont Hildur M. Fridriksdottir Gunnar B. Gudmundsson Tim J. Wright Tadashi Yamasaki Unexpected large eruptions from buoyant magma bodies within viscoelastic crust |
description |
Large-volume volcanic eruptions can occur despite only limited precursory activity. Here the authors show that modelling the combined effects of buoyant magma, viscoelastic earth behaviour, and sustained magma channels can explain such behaviour of volcanoes and gives an estimate of pressure evolution in magma bodies. |
format |
article |
author |
Freysteinn Sigmundsson Virginie Pinel Ronni Grapenthin Andrew Hooper Sæmundur A. Halldórsson Páll Einarsson Benedikt G. Ófeigsson Elías R. Heimisson Kristín Jónsdóttir Magnús T. Gudmundsson Kristín Vogfjörd Michelle Parks Siqi Li Vincent Drouin Halldór Geirsson Stéphanie Dumont Hildur M. Fridriksdottir Gunnar B. Gudmundsson Tim J. Wright Tadashi Yamasaki |
author_facet |
Freysteinn Sigmundsson Virginie Pinel Ronni Grapenthin Andrew Hooper Sæmundur A. Halldórsson Páll Einarsson Benedikt G. Ófeigsson Elías R. Heimisson Kristín Jónsdóttir Magnús T. Gudmundsson Kristín Vogfjörd Michelle Parks Siqi Li Vincent Drouin Halldór Geirsson Stéphanie Dumont Hildur M. Fridriksdottir Gunnar B. Gudmundsson Tim J. Wright Tadashi Yamasaki |
author_sort |
Freysteinn Sigmundsson |
title |
Unexpected large eruptions from buoyant magma bodies within viscoelastic crust |
title_short |
Unexpected large eruptions from buoyant magma bodies within viscoelastic crust |
title_full |
Unexpected large eruptions from buoyant magma bodies within viscoelastic crust |
title_fullStr |
Unexpected large eruptions from buoyant magma bodies within viscoelastic crust |
title_full_unstemmed |
Unexpected large eruptions from buoyant magma bodies within viscoelastic crust |
title_sort |
unexpected large eruptions from buoyant magma bodies within viscoelastic crust |
publisher |
Nature Portfolio |
publishDate |
2020 |
url |
https://doaj.org/article/0c024d3baeee4898b806085012a75a92 |
work_keys_str_mv |
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