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Isotopic and geochemical constraints on the age and origin of granitoids from the central Mawson Escarpment, southern Prince Charles Mountains, East Antarctica

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dc.contributor.authorBoger, Steven D.
dc.contributor.authorMaas, Roland
dc.contributor.authorFanning, Christopher
dc.date.accessioned2015-12-08T22:42:11Z
dc.date.issued2008
dc.date.updated2015-12-08T10:33:43Z
dc.description.abstractGranitoids from the central Mawson Escarpment (southern Prince Charles Mountains, East Antarctica) range in age from Archaean to Early Ordovician. U-Pb dating of zircon from these rocks indicates that they were emplaced in three distinct pulses: at 3,519
dc.identifier.issn0010-7999
dc.identifier.urihttp://hdl.handle.net/1885/36979
dc.publisherSpringer
dc.sourceContributions to Mineralogy and Petrology
dc.subjectKeywords: Archean; continental crust; emplacement; Gondwana; granitoid; igneous geochemistry; igneous intrusion; isotopic composition; Ordovician; orogeny; Proterozoic; SHRIMP dating; uranium-lead dating; zircon; Antarctica; East Antarctica; Prince Charles Mountain Antarctica; Gondwana; Granites; HighSr/Y; Lambert Complex; PrinceCharles Mountains; SHRIMP
dc.titleIsotopic and geochemical constraints on the age and origin of granitoids from the central Mawson Escarpment, southern Prince Charles Mountains, East Antarctica
dc.typeJournal article
local.bibliographicCitation.lastpage400
local.bibliographicCitation.startpage379
local.contributor.affiliationBoger, Steven D., University of Melbourne
local.contributor.affiliationMaas, Roland, University of Melbourne
local.contributor.affiliationFanning, Christopher, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidFanning, Christopher, u4029993
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040303 - Geochronology
local.identifier.absfor040203 - Isotope Geochemistry
local.identifier.absfor040202 - Inorganic Geochemistry
local.identifier.ariespublicationU4027924xPUB143
local.identifier.citationvolume155
local.identifier.doi10.1007/s00410-007-0249-x
local.identifier.scopusID2-s2.0-38149032946
local.identifier.thomsonID000252294400007
local.type.statusPublished Version

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