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dc.contributor.authorSoriano, Carles-
dc.contributor.authorGiordano, Daniele-
dc.contributor.authorGalindo, I.-
dc.contributor.authorHürlimann, Marcel-
dc.contributor.authorArdia, Paola-
dc.date.issued2009-04-
dc.identifier.citationBulletin of Volcanology 71(8):919–932 (2009)en_US
dc.identifier.issn0258-8900-
dc.identifier.uri10261/27534-
dc.description.abstractDuring rheomorphism subsequent to fallout deposition, a portion of the densely welded fallout of the La Grieta Member flowed back into the vent from where it was erupted, while the rest of it flowed down the outer slopes of the Las Cañadas caldera in Tenerife. The welded fallout and conduit-vent structure are physically connected and constitute a rare example of this type of deposits rooted to its feeder conduit and exposed in the caldera wall. The lower part of the vent-filling rheomorphic rocks shows gas bubbles and cavities that increase in size (up to 4 m) down vent. Bubbles are deformed against other bubbles, against the steep vent walls, flattened parallel to the flow foliation planes, and elongated parallel to the flow lineation and flow fold axes. The preservation of such giant bubbles, rather than their formation, seems to be a pretty unique feature of the phonolitic products investigated here and it is likely the result of the combination of factors that acted to preserve, in the surrounding of the glass transition interval, the sealing and the late stage cooling of a pressurized system. In addition, strain drop at the base of the vent-filling rheomorphic flow caused by flow stopping against vertical vent walls may have promoted rapid gas exsolution and the formation of large bubbles.en_US
dc.description.sponsorshipThis research has been funded by the Ministerio de Ciencia y Tecnología (MCYT) project BTE2003-08026.en_US
dc.language.isoengen_US
dc.publisherSpringeren_US
dc.rightsclosedAccessen_US
dc.subjectVolcanic venten_US
dc.subjectRheomorphismen_US
dc.subjectViscosityen_US
dc.subjectShear stressen_US
dc.titleGiant gas bubbles in a rheomorphic vent fill at the Las Cañadas caldera, Tenerife (Canary Islands)en_US
dc.typeartículoen_US
dc.identifier.doi10.1007/s00445-009-0275-9-
dc.description.peerreviewedPeer revieweden_US
dc.relation.publisherversionhttp://www.springerlink.com/content/n38753278h205128/en_US
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