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Melt- versus fluid-induced metasomatism in spinel to garnet wedge peridotites (Ulten zone, Eastern Italian alps): clues from trace element and Li abundances

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dc.contributor.authorScambelluri, Marco
dc.contributor.authorHermann, Joerg
dc.contributor.authorMorten, Lauren
dc.contributor.authorRampone, E
dc.date.accessioned2015-12-07T22:17:23Z
dc.date.issued2006
dc.date.updated2015-12-07T08:06:43Z
dc.description.abstractThe peridotite bodies of the Ulten Zone (Upper Austroalpine, Italian Eastern Alps) are enclosed in Variscan migmatites and derive from a mantle wedge environment. They display the progressive transformation of porphyroclastic spinel peridotites (T =1,200
dc.identifier.issn0010-7999
dc.identifier.urihttp://hdl.handle.net/1885/18535
dc.publisherSpringer
dc.sourceContributions to Mineralogy and Petrology
dc.subjectKeywords: lithium; metasomatism; peridotite; trace element
dc.titleMelt- versus fluid-induced metasomatism in spinel to garnet wedge peridotites (Ulten zone, Eastern Italian alps): clues from trace element and Li abundances
dc.typeJournal article
local.bibliographicCitation.lastpage394
local.bibliographicCitation.startpage372
local.contributor.affiliationScambelluri, Marco, Universita di Genova
local.contributor.affiliationHermann, Joerg, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationMorten, Lauren, Universita di Bologna
local.contributor.affiliationRampone, E, Universita di Genova
local.contributor.authoruidHermann, Joerg, u9907179
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.absfor040202 - Inorganic Geochemistry
local.identifier.ariespublicationu9503261xPUB4
local.identifier.citationvolume151
local.identifier.doi10.1007/s00410-006-0064-9
local.identifier.scopusID2-s2.0-33645030299
local.type.statusPublished Version

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