Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6752
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dc.contributor.authorallPolacci, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallMancini, L.; SYRMEP Group, Sincrotrone Trieste SCpA, Basovizza, Trieste, Italyen
dc.contributor.authorallBaker, D. R.; Earth and Planetary Sciences, McGill University, GEOTOP-UQUAM McGill Research Centre, Montreal, Canada; Sincrotrone Trieste SCpA, Basovizza, Trieste, Italyen
dc.date.accessioned2011-01-19T06:56:34Zen
dc.date.available2011-01-19T06:56:34Zen
dc.date.issued2010-03en
dc.identifier.urihttp://hdl.handle.net/2122/6752en
dc.description.abstractA series of computed microtomography experiments are reported which were performed by using a third-generation synchrotron radiation source on volcanic rocks from various active hazardous volcanoes in Italy and other volcanic areas in the world. The applied technique allowed the internal structure of the investigated material to be accurately imaged at the micrometre scale and three-dimensional views of the investigated samples to be produced as well as three-dimensional quantitative measurements of textural features. The geometry of the vesicle (gas-filled void) network in volcanic products of both basaltic and trachytic compositions were particularly focused on, as vesicle textures are directly linked to the dynamics of volcano degassing. This investigation provided novel insights into modes of gas exsolution, transport and loss in magmas that were not recognized in previous studies using solely conventional two-dimensional imaging techniques. The results of this study are important to understanding the behaviour of volcanoes and can be combined with other geosciences disciplines to forecast their future activity.en
dc.language.isoEnglishen
dc.publisher.nameInternational Union of Crystallographyen
dc.relation.ispartofJournal of Synchrotron Radiationen
dc.relation.ispartofseries2/17(2010)en
dc.relation.isversionofhttp://hdl.handle.net/2122/5766en
dc.subjecthigh-resolution three-dimensional imagingen
dc.subjectX-ray computed microtomographyen
dc.subjectvolcanic eruptionsen
dc.subjectvolcanic rock texturesen
dc.titleThe contribution of synchrotron X-ray computed microtomography to understanding volcanic processesen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber215-221en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocksen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniquesen
dc.identifier.doi10.1107/S0909049509048225en
dc.description.obiettivoSpecifico2.3. TTC - Laboratori di chimica e fisica delle rocceen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorPolacci, M.en
dc.contributor.authorMancini, L.en
dc.contributor.authorBaker, D. R.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentSYRMEP Group, Sincrotrone Trieste SCpA, Basovizza, Trieste, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptSincrotrone Trieste S.C.p.A., S.S. 14-km 163.5, 34149 Basovizza (TS), Italy-
crisitem.author.orcid0000-0003-3318-8700-
crisitem.author.orcid0000-0002-6543-3283-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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