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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6039
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dc.contributor.authorallDeegan, F. M.; DEPARTMENT OF EARTH SCIENCES, UPPSALA UNIVERSITY, VILLAVAGEN 16, 75236 UPPSALA, SWEDENen
dc.contributor.authorallTroll, V. R.; DEPARTMENT OF EARTH SCIENCES, UPPSALA UNIVERSITY, VILLAVAGEN 16, 75236 UPPSALA, SWEDENen
dc.contributor.authorallFreda, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallMisiti, V.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallChadwick, J. P.; DEPARTMENT OF PETROLOGY (FALW), VRIJE UNIVERSITEIT, 1081 HV AMSTERDAM, THE NETHERLANDSen
dc.contributor.authorallMcLeod, C. L.; DEPARTMENT OF EARTH SCIENCES, THE UNIVERSITY OF DURHAM, DURHAM DH1 3LE, UKen
dc.contributor.authorallDavidson, J. P.; DEPARTMENT OF EARTH SCIENCES, THE UNIVERSITY OF DURHAM, DURHAM DH1 3LE, UKen
dc.date.accessioned2010-06-11T10:55:29Zen
dc.date.available2010-06-11T10:55:29Zen
dc.date.issued2010-02-25en
dc.identifier.urihttp://hdl.handle.net/2122/6039en
dc.description.abstractThere is considerable evidence for continuing, late-stage interaction between the magmatic system at Merapi volcano, Indonesia, and local crustal carbonate (limestone). Calc-silicate xenoliths within Merapi basaltic-andesite eruptive rocks display textures indicative of intense interaction between magma and crustal carbonate, and Merapi feldspar phenocrysts frequently contain crustally contaminated cores and zones. To resolve the interaction processes between magma and limestone in detail we have performed a series of time-variable decarbonation experiments in silicate melt, at magmatic pressure and temperature, using a Merapi basaltic-andesite and local Javanese limestone as starting materials.We have used in situ analytical methods to determine the elemental and strontium isotope composition of the experimental products and to trace the textural, chemical, and isotopic evolution of carbonate assimilation. The major processes of magma^carbonate interaction identified are: (1) rapid decomposition and degassing of carbonate; (2) generation of a Ca-enriched, highly radiogenic strontium contaminant melt, distinct from the starting material composition; (3) intense CO2 vesiculation, particularly within the contaminated zones; (4) physical mingling between the contaminated and unaffected melt domains; (5) chemical mixing between melts. The experiments reproduce many of the features of magma^carbonate interaction observed in the natural Merapi xenoliths and feldspar phenocrysts. The Ca-rich, high 87Sr/86Sr contaminant melt produced in the experiments is considered as a precursor to the Ca-rich (often ‘hyper-calcic’) phases found in the xenoliths and the contaminated zones inMerapi feldspars.The xenoliths also exhibit micro-vesicular textures that can be linked to the CO2 liberation process seen in the experiments.This study, therefore, provides well-constrained petrological insights into the problem of crustal interaction at Merapi and points toward the substantial impact of such interaction on the volatile budget of the volcano.en
dc.description.sponsorshipSwedish Science Foundation (Vetenskapsrdet) Project FIRBMIUR‘Development of innovative technologies for the environmental protection fromnatural events’en
dc.language.isoEnglishen
dc.relation.ispartofJournal of Petrologyen
dc.relation.ispartofseries5/51(2010)en
dc.subjectcarbon dioxideen
dc.subjectexperimental petrologyen
dc.subjectmagma-carbonate interactionen
dc.subjectMerapien
dc.subject; strontium isotopesen
dc.titleMagma-Carbonate Interaction Processes and Associated CO2 Release at MerapiVolcano, Indonesia: Insights from Experimental Petrologyen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1027-1051en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.03. Magmasen
dc.identifier.doi10.1093/petrology/egq010en
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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.authorDeegan, F. M.en
dc.contributor.authorTroll, V. R.en
dc.contributor.authorFreda, C.en
dc.contributor.authorMisiti, V.en
dc.contributor.authorChadwick, J. P.en
dc.contributor.authorMcLeod, C. L.en
dc.contributor.authorDavidson, J. P.en
dc.contributor.departmentDEPARTMENT OF EARTH SCIENCES, UPPSALA UNIVERSITY, VILLAVAGEN 16, 75236 UPPSALA, SWEDENen
dc.contributor.departmentDEPARTMENT OF EARTH SCIENCES, UPPSALA UNIVERSITY, VILLAVAGEN 16, 75236 UPPSALA, SWEDENen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentDEPARTMENT OF PETROLOGY (FALW), VRIJE UNIVERSITEIT, 1081 HV AMSTERDAM, THE NETHERLANDSen
dc.contributor.departmentDEPARTMENT OF EARTH SCIENCES, THE UNIVERSITY OF DURHAM, DURHAM DH1 3LE, UKen
dc.contributor.departmentDEPARTMENT OF EARTH SCIENCES, THE UNIVERSITY OF DURHAM, DURHAM DH1 3LE, UKen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartment of Geosciences, Swedish Museum of Natural History-
crisitem.author.deptUppsala University-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptDEPARTMENT OF PETROLOGY (FALW), VRIJE UNIVERSITEIT, 1081 HV AMSTERDAM, THE NETHERLANDS-
crisitem.author.deptDepartment of Earth Sciences, Durham University,-
crisitem.author.deptDEPARTMENT OF EARTH SCIENCES, THE UNIVERSITY OF DURHAM, DURHAM DH1 3LE, UK-
crisitem.author.orcid0000-0002-9065-9225-
crisitem.author.orcid0000-0003-1891-3396-
crisitem.author.orcid0000-0002-2320-8096-
crisitem.author.orcid0000-0002-6151-7789-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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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