Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7429
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dc.contributor.authorallFerrando, S.; Dipartimento di Scienze della Terra, Università di Sienaen
dc.contributor.authorallFrezzotti, M. L.; Dipartimento di Scienze della Terra, Università di Sienaen
dc.contributor.authorallNeumann, E. R.; Physics of Geological Processes, University of Osloen
dc.contributor.authorallDe Astis, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallPeccerillo, A.; Dipartimento di Scienze della Terra, Università di Perugiaen
dc.contributor.authorallDereje, A.; Department of Geology and Geophysics, Faculty of Science, Addis Ababa Universityen
dc.contributor.authorallGezahegn, Y.; Department of Geology and Geophysics, Faculty of Science, Addis Ababa Universityen
dc.contributor.authorallTeklewold, A.en
dc.date.accessioned2012-01-19T14:46:38Zen
dc.date.available2012-01-19T14:46:38Zen
dc.date.issued2008en
dc.identifier.urihttp://hdl.handle.net/2122/7429en
dc.description.abstractPetrographic, minerochemical, and geothermobarometric data are reported for a suite of spinel-lherzolite pargasite xenoliths hosted in a Quaternary basanitic lava flow from the North-Western Ethiopian Plateau (Injibara, Lake Tana Province). Protogranular to porphyroclastic (deformed) rocks show evidence of a modal metasomatism, represented by a Cl-rich pargasitic amphibole, coupled with cryptic enrichment in Fe and Al. Equigranular rocks (granular) record a further cryptic metasomatism, represented by enrichment in Fe, Al, Na, and depletion in Ni, Cr and Cl. Some xenoliths (transitional) show intermediate textural and compositional characters, indicating that the granular samples represent an evolution of the deformed ones. All xenoliths give the same P–T equilibration conditions for Opx-Cpx pairs (947–1015 C and 1.3–2.0 GPa), but in granular samples, recrystallised olivine and spinel record T about 100 C higher. Two distinct metasomatic processes, probably connected with the emplacement of the Afar plume, are proposed. The first one is a pervasive modal metasomatism produced by water-rich fluids. The latter is a non-pervasive cryptic metasomatism, probably connected to migration of melts. The comparison the mantle beneath the Ethiopian Volcanic Plateau, the southern Main Ethiopian Rift and the central Main Ethiopian Rift suggests spatial heterogeneity of the mantle and variable mantle processes during asthenospheric upwelling.en
dc.language.isoEnglishen
dc.publisher.nameSpringer-Verlagen
dc.relation.ispartofMineralogy and Petrologyen
dc.relation.ispartofseries/93 (2008)en
dc.relation.isversionofhttp://hdl.handle.net/2122/2865en
dc.subjectlithosphereen
dc.subjectperidotite xenolithsen
dc.subjectEthiopian Volcanic Plateauen
dc.subjectMetasomatismen
dc.titleComposition and thermal structure of the lithosphere beneath the Ethiopian plateau: evidence from mantle xenoliths in basanites, Injibara, Lake Tana Provinceen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber47-78en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrologyen
dc.identifier.doi10.1007/s00710-007-0219-zen
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dc.description.obiettivoSpecifico3.3. Geodinamica e struttura dell'interno della Terraen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorFerrando, S.en
dc.contributor.authorFrezzotti, M. L.en
dc.contributor.authorNeumann, E. R.en
dc.contributor.authorDe Astis, G.en
dc.contributor.authorPeccerillo, A.en
dc.contributor.authorDereje, A.en
dc.contributor.authorGezahegn, Y.en
dc.contributor.authorTeklewold, A.en
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Sienaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Sienaen
dc.contributor.departmentPhysics of Geological Processes, University of Osloen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Perugiaen
dc.contributor.departmentDepartment of Geology and Geophysics, Faculty of Science, Addis Ababa Universityen
dc.contributor.departmentDepartment of Geology and Geophysics, Faculty of Science, Addis Ababa Universityen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Siena-
crisitem.author.deptUniversità di Milano Bicocca-
crisitem.author.deptPhysics of Geological Processes, University of Oslo, Norway-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptDipartimento di Scienze della Terra, Universita` di Perugia, Piazza Universita` , I-06100 Perugia, Italy-
crisitem.author.deptDepartment of Geology and Geophysics, Faculty of Science, Addis Ababa University-
crisitem.author.deptDepartment of Geology and Geophysics, Faculty of Science, Addis Ababa University-
crisitem.author.deptDepartment of Geology and Geophysics,Addis Ababa University, Ethiopia-
crisitem.author.orcid0000-0002-6992-8259-
crisitem.author.orcid0000-0003-2057-1276-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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