Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5511
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dc.contributor.authorallGaeta, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallDi Rocco, T.; Università di Roma La sapienzaen
dc.contributor.authorallFreda, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2010-01-11T09:57:48Zen
dc.date.available2010-01-11T09:57:48Zen
dc.date.issued2009-01-21en
dc.identifier.urihttp://hdl.handle.net/2122/5511en
dc.description.abstractThe geochemical characteristics of volcanic products in a variety of tectonic settings demonstrate that incorporation of crustal material into magmas is a relatively common process. Contamination of magmas by crustal components, in turn, can have a significant effect on magma composition and rheology. Despite this, the mechanism by which contamination occurs is still not well established and its efficacy is denied by some. In this study we focus on magma^ carbonate interaction and on the rock shells (cumulates and skarns) formed at the contact between a magma chamber and its wall-rocks.We deduce that previous, unsuccessful attempts at carbonate assimilation^fractional crystallization (AFC) modelling can be related to the paucity of information about the cumulate zone in contact with skarns.We use one of the best examples of a magmatic plumbing system emplaced within a thick carbonate substratum (the Colli AlbaniVolcanic District in Central Italy) to demonstrate that a ‘skarn environment’can act as a source of CaO-rich silicate melts, and that the assimilation of these melts into the primitive magma is the main process responsible for magma contamination, rather than the ingestion of solid carbonate wall-rocks. In particular, by means of microtextural observations, mineral chemistry, whole-rock geochemical data and MELTS simulations we highlight the effect of high Ca-Tschermaks (CaAl2SiO6) activity in the melt on the stability of Cr-spinel, olivine, and clinopyroxene in cumulate rocks, define a reaction-cumulate zone where clinopyroxene crystallization is favoured, and model the magmatic differentiation processes active in this zone.en
dc.description.sponsorshipINGV-DPC Project V3_1 Colli Albani MIUR ‘Caratteristiche vulcanologiche e geomeccaniche dei prodotti recenti dei Colli Albani’.en
dc.language.isoEnglishen
dc.relation.ispartofJournal of Petrologyen
dc.relation.ispartofseries2/50 (2009)en
dc.subjectcumulateen
dc.subjectcarbonate assimilationen
dc.subjectopen systemen
dc.subjectColli Albanien
dc.titleCarbonate assimilation in open magmatic systems: the role of melt-bearing skarns and cumulate-forming processesen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber361-385en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.03. Magmasen
dc.identifier.doi10.1093/petrology/egp002en
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dc.description.obiettivoSpecifico2.3. TTC - Laboratori di chimica e fisica delle rocceen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorGaeta, M.en
dc.contributor.authorDi Rocco, T.en
dc.contributor.authorFreda, C.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentUniversità di Roma La sapienzaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità La Sapienza-
crisitem.author.deptUniversità di Roma La sapienza-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-2320-8096-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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