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Natures diffusion experiment: The cooling-rate cooling-age correlation

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dc.contributor.authorDunlap, William James
dc.date.accessioned2015-12-13T23:15:19Z
dc.date.available2015-12-13T23:15:19Z
dc.date.issued2000
dc.date.updated2016-02-24T09:48:18Z
dc.description.abstractCorrelation between the age of orogeny and the cooling rate of metamorphic rocks (through ∼ 500-180 °C), as determined through various radioisotopic dating methods, suggests that ancient orogens cooled at rates as much as two orders of magnitude slower
dc.identifier.issn0091-7613
dc.identifier.urihttp://hdl.handle.net/1885/88853
dc.publisherGeological Society of America Inc
dc.sourceGeology
dc.subjectKeywords: cooling; exhumation; geochronology; orogeny Argon; Biotite; Cooling; Diffusion; Exhumation
dc.titleNatures diffusion experiment: The cooling-rate cooling-age correlation
dc.typeJournal article
local.bibliographicCitation.issue2
local.bibliographicCitation.lastpage142
local.bibliographicCitation.startpage139
local.contributor.affiliationDunlap, William James, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidDunlap, William James, u9505456
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor080605 - Decision Support and Group Support Systems
local.identifier.ariespublicationMigratedxPub18711
local.identifier.citationvolume28
local.identifier.doi10.1130/0091-7613(2000)28<139:NDETCC>2.0.CO
local.identifier.scopusID2-s2.0-84874998563
local.type.statusPublished Version

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