Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6775
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dc.contributor.authorallZandomeneghi, D.; International Centre for Theoretical Physics, Trieste, Italyen
dc.contributor.authorallVoltolini, M.; Sincrotrone Trieste S.C.p.A., Basovizza, Trieste, Italyen
dc.contributor.authorallMancini, L.; Sincrotrone Trieste S.C.p.A., Basovizza, Trieste, Italyen
dc.contributor.authorallBrun, F.; Sincrotrone Trieste S.C.p.A., Basovizza, Trieste, Italy; Dipartimento di Elettronica, Elettrotecnica ed Informatica, Universitá di Trieste, Trieste, Italyen
dc.contributor.authorallDreossi, D.; Sincrotrone Trieste S.C.p.A., Basovizza, Trieste, Italyen
dc.contributor.authorallPolacci, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.date.accessioned2011-01-20T07:41:58Zen
dc.date.available2011-01-20T07:41:58Zen
dc.date.issued2010-12en
dc.identifier.urihttp://hdl.handle.net/2122/6775en
dc.description.abstractX-ray computed microtomography is an excellent tool for the three-dimensional analysis of rock microstructure. Digital images are acquired, visualized, and processed to identify and measure several discrete features and constituents of rock samples, by means of mathematical algorithms and computational methods. In this paper, we present digital images of volcanic rocks collected with X-ray computed microtomography techniques and studied by means of a software library, called Pore3D, custom-implemented at the Elettra Synchrotron Light Laboratory of Trieste (Italy). Using the Pore3D software, we analyzed the fabrics and we quantified the characteristics of the main constituents (vesicles, crystals, and glassy matrix) of four different types of pyroclasts: frothy pumice, tube pumice, scoria, and “crystalline” scoria. We identified the distinctive features of these different types of volcanic rocks. The frothy pumices show vesicles that coalesce in isotropic aggregates, especially toward the sample interior, while the scoriae have a low porosity and an abundance of isolated vesicles. In the “crystalline” scoria sample most of the vesicle separation is due to the presence of crystals of different types, while the tube pumice shows an anisotropic distribution of vesicles and crystals at the microscale, as also observed at the scale of the hand sample. Quantitative analysis and textural information may supply an additional tool to investigate the eruptive processes and the origin of volcanic rocks.en
dc.language.isoEnglishen
dc.publisher.nameGeological Society of Americaen
dc.relation.ispartofGeosphereen
dc.relation.ispartofseries6/6(2010)en
dc.subjectX-ray tomographyen
dc.subject3D imagingen
dc.subjectvolcanic rocksen
dc.titleQuantitative analysis of X-ray microtomography images of geomaterials: Application to volcanic rocksen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber793-804en
dc.identifier.URLhttp://geosphere.gsapubs.org/content/6/6/793.fullen
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.doi10.1130/GES00561.1en
dc.description.obiettivoSpecifico2.3. TTC - Laboratori di chimica e fisica delle rocceen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorZandomeneghi, D.en
dc.contributor.authorVoltolini, M.en
dc.contributor.authorMancini, L.en
dc.contributor.authorBrun, F.en
dc.contributor.authorDreossi, D.en
dc.contributor.authorPolacci, M.en
dc.contributor.departmentInternational Centre for Theoretical Physics, Trieste, Italyen
dc.contributor.departmentSincrotrone Trieste S.C.p.A., Basovizza, Trieste, Italyen
dc.contributor.departmentSincrotrone Trieste S.C.p.A., Basovizza, Trieste, Italyen
dc.contributor.departmentSincrotrone Trieste S.C.p.A., Basovizza, Trieste, Italy; Dipartimento di Elettronica, Elettrotecnica ed Informatica, Universitá di Trieste, Trieste, Italyen
dc.contributor.departmentSincrotrone Trieste S.C.p.A., Basovizza, Trieste, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptInstituto Andaluz de Geofísica, Universidad de Granada, Granada, Spain-
crisitem.author.deptSincrotrone Trieste S.C.p.A., Basovizza, Trieste, Italy-
crisitem.author.deptSincrotrone Trieste S.C.p.A., S.S. 14-km 163.5, 34149 Basovizza (TS), Italy-
crisitem.author.deptSincrotrone Trieste S.C.p.A., Basovizza, Trieste, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.orcid0000-0003-0155-5326-
crisitem.author.orcid0000-0003-3318-8700-
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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