Volcanotectonics: the tectonics and physics of volcanoes and their eruption mechanics

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dc.catalogadorjca
dc.contributor.authorGudmundsson, Agust
dc.contributor.authorDrymoni, Kyriaki
dc.contributor.authorBrowning, John
dc.contributor.authorAcocella, Valerio
dc.contributor.authorAmelung, Falk
dc.contributor.authorBonali, Fabio L.
dc.contributor.authorElshaafi, Abdelsalam
dc.contributor.authorGalindo, Ines
dc.contributor.authorGeshi, Nobuo
dc.contributor.authorGeyer, Adelina
dc.contributor.authorHeap, Michael J.
dc.contributor.authorKaraoğlu, Özgür
dc.contributor.authorKusumoto, Shigekazu
dc.contributor.authorMarti, Joa
dc.contributor.authorPinel, Virginie
dc.contributor.authorTibaldi, Alessandro
dc.contributor.authorThordarson, Thorvaldur
dc.contributor.authorWalter, Thomas R.
dc.date.accessioned2024-06-06T14:28:08Z
dc.date.available2024-06-06T14:28:08Z
dc.date.issued2022
dc.description.abstractThe physical processes that operate within, and beneath, a volcano control the frequency, duration, location and size of volcanic eruptions. Volcanotectonics focuses on such processes, combining techniques, data, and ideas from structural geology, tectonics, volcano deformation, physical volcanology, seismology, petrology, rock and fracture mechanics and classical physics. A central aim of volcanotectonics is to provide sufficient understanding of the internal processes in volcanoes so that, when combined with monitoring data, reliable forecasting of eruptions, vertical (caldera) and lateral (landslide) collapses and related events becomes possible. To gain such an understanding requires knowledge of the material properties of the magma and the crustal rocks, as well as the associated stress fields, and their evolution. The local stress field depends on the properties of the layers that constitute the volcano and, in particular, the geometric development of its shallow magma chamber. During this decade an increasing use of data from InSAR, pixel offset and structure-from-motion, as well as dense, portable seismic networks will provide further details on the mechanisms of volcanic unrest, magma-chamber rupture, the propagation of magma-filled fractures (dikes, inclined sheets and sills) and lateral and vertical collapse. Additionally, more use will be made of accurate quantitative data from fossil and active volcanoes, combined with realistic numerical, analytical and machine-learning studies, so as to provide reliable models on volcano behaviour and eruption forecasting.
dc.fuente.origenORCID
dc.identifier.doi10.1007/s00445-022-01582-4
dc.identifier.issn1432-0819
dc.identifier.urihttps://doi.org/10.1007/s00445-022-01582-4
dc.identifier.urihttps://link.springer.com/article/10.1007/s00445-022-01582-4
dc.identifier.urihttps://repositorio.uc.cl/handle/11534/86499
dc.information.autorucEscuela de Ingeniería; Browning , John; 0000-0001-8022-6234; 1081089
dc.issue.numero72
dc.language.isoen
dc.nota.accesocontenido completo
dc.pagina.final8
dc.pagina.inicio1
dc.revistaBulletin of Volcanology
dc.rightsacceso abierto
dc.subjectVolcano monitoring
dc.subjectMagma-chamber
dc.subjectMagma plumbing system
dc.subjectDike propagation
dc.subjectCaldera collapse
dc.subjectEruption forecast
dc.subject.ddc550
dc.subject.deweyCiencias de la tierraes_ES
dc.titleVolcanotectonics: the tectonics and physics of volcanoes and their eruption mechanics
dc.typeartículo
dc.volumen84
sipa.codpersvinculados1081089
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