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Isotopic test of a thermally driven intraplate orogenic model, Australia

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dc.contributor.authorCamacho, A
dc.contributor.authorHensen, Bas
dc.contributor.authorArmstrong, Richard
dc.date.accessioned2015-12-13T22:22:18Z
dc.date.available2015-12-13T22:22:18Z
dc.date.issued2002
dc.date.updated2015-12-11T07:55:11Z
dc.description.abstractA recently proposed model for intraplate orogenesis couples long-term self-heating of basement rocks by radioactive decay with thermal blanketing by overlying sedimentary deposits. This model has been tested in one of the type areas in central Australia,
dc.identifier.issn0091-7613
dc.identifier.urihttp://hdl.handle.net/1885/72194
dc.publisherGeological Society of America Inc
dc.sourceGeology
dc.subjectKeywords: Thermal blanketing; Geologic models; Radioactivity; Sedimentation; Geology; intraplate process; metamorphism; orogeny; provenance; tectonic evolution; thermal evolution; Australia Metamorphism; Provenance; Tectonics; Thermal disequilibrium
dc.titleIsotopic test of a thermally driven intraplate orogenic model, Australia
dc.typeJournal article
local.bibliographicCitation.issue10
local.bibliographicCitation.lastpage890
local.bibliographicCitation.startpage887
local.contributor.affiliationCamacho, A, University of New South Wales
local.contributor.affiliationHensen, Bas, University of New South Wales
local.contributor.affiliationArmstrong, Richard, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidArmstrong, Richard, u4029979
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040313 - Tectonics
local.identifier.absfor040303 - Geochronology
local.identifier.ariespublicationMigratedxPub3109
local.identifier.citationvolume30
local.identifier.doi10.1130/0091-7613(2002)030<0887:ITOATD>2.0.CO;2
local.identifier.scopusID2-s2.0-0036808585
local.type.statusPublished Version

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