Identification and elimination of a matrix-induced systematic error in LA-ICP-MS 206pB/238u dating of zircon

dc.contributor.authorAllen, Charlotte M
dc.contributor.authorCampbell, Ian
dc.date.accessioned2015-12-08T22:23:03Z
dc.date.issued2012
dc.date.updated2016-02-24T11:40:36Z
dc.description.abstractLink references in abstract. Black et al. (2004) identified a systematic difference between LA-ICP-MS and TIMS measurements of 206Pb/ 238U in zircons, which they correlated with the incompatible trace element content of the zircon. We show that the offset between the LA-ICP-MS and TIMS measured 206Pb/ 238U correlates more strongly with the total radiogenic Pb than with any incompatible trace element. This suggests that the cause of the 206Pb/ 238U offset is related to differences in the radiation damage (alpha dose) between the reference and unknowns. We test this hypothesis in two ways. First, we show that there is a strong correlation between the difference in the LA-ICP-MS and TIMS measured 206Pb/ 238U and the difference in the alpha dose received by unknown and reference zircons. The LA-ICP-MS ages for the zircons we have dated can be as much as 5.1% younger than their TIMS age to 2.1% older, depending on whether the unknown or reference received the higher alpha dose. Second, we show that by annealing both reference and unknown zircons at 850°C for 48h in air we can eliminate the alpha-dose-induced differences in measured 206Pb/ 238U. This was achieved by analyzing six reference zircons a minimum of 16 times in two round robin experiments: the first consisting of unannealed zircons and the second of annealed grains. The maximum offset between the LA-ICP-MS and TIMS measured 206Pb/ 238U for the unannealed zircons was 2.3%, which reduced to 0.5% for the annealed grains, as predicted by within-session precision based on counting statistics. Annealing unknown zircons and references to the same state prior to analysis holds the promise of reducing the 3% external error for the measurement of 206Pb/ 238U of zircon by LA-ICP-MS, indicated by Klötzli et al. (2009), to better than 1%, but more analyses of annealed zircons by other laboratories are required to evaluate the true potential of the annealing method.
dc.identifier.issn0009-2541
dc.identifier.urihttp://hdl.handle.net/1885/32704
dc.publisherElsevier
dc.sourceChemical Geology
dc.subjectKeywords: Accuracy; ICP-MS; Matrix effects; Precision; SHRIMP; Annealing; Geochronology; Lead; Mass spectrometers; Radiation damage; Thermal insulating materials; Zircon; Inductively coupled plasma mass spectrometry; accuracy assessment; age determination; annealin Accuracy; ICP-MS; Matrix effect; Precision; SHRIMP; U/Pb zircon geochronology
dc.titleIdentification and elimination of a matrix-induced systematic error in LA-ICP-MS 206pB/238u dating of zircon
dc.typeJournal article
local.bibliographicCitation.lastpage165
local.bibliographicCitation.startpage157
local.contributor.affiliationAllen, Charlotte M, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationCampbell, Ian, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidAllen, Charlotte M, u9108301
local.contributor.authoruidCampbell, Ian, u8300206
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040303 - Geochronology
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationU8501506xPUB94
local.identifier.citationvolume332-333
local.identifier.doi10.1016/j.chemgeo.2012.09.038
local.identifier.scopusID2-s2.0-84867585374
local.identifier.thomsonID000313767100014
local.type.statusPublished Version

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