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(2008) The feasibility of generating low-frequency volcano seismicity by flow through a deformable channel. Special Publication, 307. Geological Society of London. 45-56 doi:10.1144/sp307.4

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Reference TypeReport (article/chapter)
TitleThe feasibility of generating low-frequency volcano seismicity by flow through a deformable channel
ReportSpecial Publication
Year2008Volume307
PublisherGeological Society of London
DOIdoi:10.1144/sp307.4Search in ResearchGate
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Mindat Ref. ID435720Long-form Identifiermindat:1:5:435720:3
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Full Reference(2008) The feasibility of generating low-frequency volcano seismicity by flow through a deformable channel. Special Publication, 307. Geological Society of London. 45-56 doi:10.1144/sp307.4
Plain Text(2008) The feasibility of generating low-frequency volcano seismicity by flow through a deformable channel. Special Publication, 307. Geological Society of London. 45-56 doi:10.1144/sp307.4
In(2008) Special Publication Vol. 307. Geological Society of London

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(2008) Special Publication, 307. Geological Society of London. doi:10.1144/sp307
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(2011) Discontinuous low-velocity zones in southern Tibet question the viability of the channel flow model. Special Publication, 353. Geological Society of London. 99-108 doi:10.1144/sp353.6
(2008) From Strombolian explosions to fire fountains at Etna Volcano (Italy): what do we learn from acoustic measurements?. Special Publication, 307. Geological Society of London. 103-124 doi:10.1144/sp307.7
 
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