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Silicon-32 as a tool for dating the recent past

Fifield, L Keith; Morgenstern, Uwe

Description

Silicon-32, with a half-life of approximately 140 years, has the potential to fill the dating gap that lies between those chronologies based on the shorter-lived isotopes of 3H and 210Pb, and those based on the longer-lived 14C. Silicon-32 is produced in

dc.contributor.authorFifield, L Keith
dc.contributor.authorMorgenstern, Uwe
dc.date.accessioned2015-12-10T22:32:10Z
dc.identifier.issn1871-1014
dc.identifier.urihttp://hdl.handle.net/1885/55640
dc.description.abstractSilicon-32, with a half-life of approximately 140 years, has the potential to fill the dating gap that lies between those chronologies based on the shorter-lived isotopes of 3H and 210Pb, and those based on the longer-lived 14C. Silicon-32 is produced in
dc.publisherElsevier
dc.sourceQuaternary Geochronology
dc.subjectKeywords: chronology; concentration (composition); dating method; half life; measurement method; silicon Accelerator mass spectrometry; Dating; Radiometric counting; Recent past; Silicon-32
dc.titleSilicon-32 as a tool for dating the recent past
dc.typeJournal article
local.description.notesImported from ARIES
local.identifier.citationvolume4
dc.date.issued2009
local.identifier.absfor040303 - Geochronology
local.identifier.ariespublicationu4155331xPUB335
local.type.statusPublished Version
local.contributor.affiliationFifield, L Keith, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationMorgenstern, Uwe, GNS Science
local.description.embargo2037-12-31
local.bibliographicCitation.startpage400
local.bibliographicCitation.lastpage405
local.identifier.doi10.1016/j.quageo.2008.12.006
dc.date.updated2016-02-24T10:38:42Z
local.identifier.scopusID2-s2.0-69749109635
local.identifier.thomsonID000271335200008
CollectionsANU Research Publications

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