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Sub-solidus Oligocene zircon formation in garnet peridotite during fast decompression and fluid infiltration (Duria, Central Alps)

dc.contributor.authorHermann, Joerg
dc.contributor.authorRubatto, Daniela
dc.contributor.authorTrommsdorff, Volkmar
dc.date.accessioned2015-12-07T22:20:57Z
dc.date.issued2006
dc.date.updated2015-12-07T08:52:24Z
dc.description.abstractA garnet peridotite lens from Monte Duria (Adula nappe, Central Alps, Northern Italy) contains porphyroblastic garnet and pargasitic amphibole and reached peak metamorphic conditions of ∼830°C, ∼2.8 GPa. A first stage of near isothermal decompression
dc.identifier.issn0930-0708
dc.identifier.urihttp://hdl.handle.net/1885/19813
dc.publisherSpringer
dc.sourceMineralogy and Petrology
dc.titleSub-solidus Oligocene zircon formation in garnet peridotite during fast decompression and fluid infiltration (Duria, Central Alps)
dc.typeJournal article
local.bibliographicCitation.lastpage206
local.bibliographicCitation.startpage181
local.contributor.affiliationHermann, Joerg, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationRubatto, Daniela, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationTrommsdorff, Volkmar, Swiss Federal Institute of Technology (ETH)
local.contributor.authoruidHermann, Joerg, u9907179
local.contributor.authoruidRubatto, Daniela, u9909045
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040203 - Isotope Geochemistry
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.ariespublicationu9503261xPUB9
local.identifier.citationvolume88
local.identifier.doi10.1007/s00710-006-0155-3
local.identifier.scopusID2-s2.0-33748278537
local.type.statusPublished Version

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