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dc.contributor.authorNobile, A.
dc.contributor.authorAcocella, V.
dc.contributor.authorRuch, J.
dc.contributor.authorAoki, Y.
dc.contributor.authorBorgstrom, S.
dc.contributor.authorSiniscalchi, V.
dc.contributor.authorGeshi, N.
dc.contributor.editorK.V. Cashman
dc.coverage.spatialJapan
dc.coverage.temporal1996-2011
dc.date2017
dc.date.accessioned2024-03-14T13:14:37Z
dc.date.available2024-03-14T13:14:37Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/11918
dc.descriptionThe relation between unrest and eruption at calderas is still poorly understood. Aso caldera, Japan, shows minor episodic phreatomagmatic eruptions associated with steady subsidence. We analyse the deformation of Aso using SAR images from 1993 to 2011 and compare it with the eruptive activity. Although the dataset suffers from limitations (e.g. atmospheric effects, coherence loss, low signal-to-noise ratio), we observe a steady subsidence signal from 1996 to 1998, which suggests an overall contraction of a magmatic source below the caldera centre, from 4 to 5 km depth. We propose that the observed contraction may have been induced by the release of the magmatic fluids feeding the eruptions. If confirmed by further data, this hypothesis suggests that degassing processes play a crucial role in triggering minor eruptions within open conduit calderas, such as at Aso. Our study underlines the importance of defining any eruptive potential also from deflating magmatic systems with open conduit.
dc.languageeng
dc.publisherSpringer
dc.titleSteady subsidence of a repeatedly erupting caldera through InSAR observations: Aso, Japan
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeNatural hazards
dc.source.titleBulletin of Volcanology
dc.source.volume79:32
Orfeo.peerreviewedYes
dc.identifier.doi10.1007/s00445-017-1112-1
dc.identifier.rmca4981


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