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Tracing Archaean terranes under Greenland's Icecap: U-Th-Pb-Hf isotopic study of zircons from melt-water rivers in the Isua area

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dc.contributor.authorYi, Keewok
dc.contributor.authorBennett, Victoria
dc.contributor.authorNutman, Allen P.
dc.contributor.authorLee, Seung Ryeol
dc.date.accessioned2015-12-13T22:34:53Z
dc.date.issued2014
dc.date.updated2015-12-11T09:24:39Z
dc.description.abstractThe Archaean gneisses of the Nuuk area (southern West Greenland) are partitioned into tectonostratigraphic terranes - blocks of arc-like crust that evolved independently until they coalesced by collisional orogeny. To 'map' terranes to the east under the
dc.identifier.issn0301-9268
dc.identifier.urihttp://hdl.handle.net/1885/76332
dc.publisherElsevier
dc.sourcePrecambrian Research
dc.titleTracing Archaean terranes under Greenland's Icecap: U-Th-Pb-Hf isotopic study of zircons from melt-water rivers in the Isua area
dc.typeJournal article
local.bibliographicCitation.issueP3
local.bibliographicCitation.lastpage921
local.bibliographicCitation.startpage900
local.contributor.affiliationYi, Keewok, Korea Basic Science Institute
local.contributor.affiliationBennett, Victoria, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationNutman, Allen P., University of Wollongong
local.contributor.affiliationLee, Seung Ryeol, Korean Institute of Geoscience and Mineral Resources
local.contributor.authoruidBennett, Victoria, u8904005
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040203 - Isotope Geochemistry
local.identifier.absfor040303 - Geochronology
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationU3488905xPUB5158
local.identifier.citationvolume255
local.identifier.doi10.1016/j.precamres.2014.04.006
local.identifier.scopusID2-s2.0-84918831878
local.identifier.thomsonID000347660600009
local.type.statusPublished Version

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