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    <title>UTas ePrints - U-Pb dating of zircon by LA-ICP-MS</title>
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    <meta content="Chang, Z." name="eprints.creators_name" />
<meta content="Vervoort, J. D." name="eprints.creators_name" />
<meta content="McClelland, W. C." name="eprints.creators_name" />
<meta content="Knaack, C." name="eprints.creators_name" />
<meta content="zhaoshan.chang@utas.edu.au" name="eprints.creators_id" />
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<meta content="2007-02-08" name="eprints.datestamp" />
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<meta content="U-Pb dating of zircon by LA-ICP-MS" name="eprints.title" />
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<meta content="laser ablation; magnetic sector ICP-MS; U-Pb dating; zircon dating." name="eprints.keywords" />
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<meta content="In this study we used LA-ICP-MS (laser ablation-inductively coupled plasma-mass spectrometry) to
determine U-Pb ages of 5 zircon samples of known age (1800 Ma to 50 Ma) in order to determine the
reproducibility, precision, and accuracy of this geochronologic technique. This work was performed using
a ThermoFinnigan Element2 magnetic sector double-focusing ICP-MS coupled with a New Wave
Research UP-213 laser system. The laser ablation pit sizes ranged from 30 to 40 mm in diameter. Laserinduced
time-dependent fractionation is corrected by normalizing measured ratios in both standards and
samples to the beginning of the analysis using the intercept method. Static fractionation, including those
caused during laser ablation and due to instrumental discrimination, is corrected using external zircon
standards. Total uncertainty for each laser analysis of an unknown is combined quadratically from the
uncertainty in the measured isotope ratios of the unknown and the uncertainty in the fractionation factors
calculated from the measurement of standards. For individual analyses we estimate that the accuracy and
precision are better than 4% at the 2 sigma level, with the largest contribution in uncertainty from the
measurement of the standards. Accuracy of age determinations in this study is on the order of 1% on the
basis of comparing the weighted average of the LA-ICP-MS determinations to the TIMS ages. Due to
unresolved contributions to uncertainty from the lack of a common Pb correction and from potential matrix
effects between standards and unknowns, however, this estimate cannot be universally applied to all
unknowns. Nevertheless, the results of this study provide an example of the type of precision and accuracy
that may be possible with this technique under ideal conditions. In summary, the laser ablation technique,
using a magnetic sector ICP-MS, can be used for the U-Pb dating of zircons with a wide range of ages and
is a useful complement to the established TIMS and SHRIMP techniques. This technique is especially well
suited to reconnaissance geochronologic and detrital zircon studies." name="eprints.abstract" />
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<meta content="Chang, Z. and Vervoort, J. D. and McClelland, W. C. and Knaack, C. (2006) U-Pb dating of zircon by LA-ICP-MS. Geochemistry Geophysics Geosystems, 7 (5). ISSN 1525-2027" name="eprints.citation" />
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<meta content="Chang, Z." name="DC.creator" />
<meta content="Vervoort, J. D." name="DC.creator" />
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<meta content="In this study we used LA-ICP-MS (laser ablation-inductively coupled plasma-mass spectrometry) to
determine U-Pb ages of 5 zircon samples of known age (1800 Ma to 50 Ma) in order to determine the
reproducibility, precision, and accuracy of this geochronologic technique. This work was performed using
a ThermoFinnigan Element2 magnetic sector double-focusing ICP-MS coupled with a New Wave
Research UP-213 laser system. The laser ablation pit sizes ranged from 30 to 40 mm in diameter. Laserinduced
time-dependent fractionation is corrected by normalizing measured ratios in both standards and
samples to the beginning of the analysis using the intercept method. Static fractionation, including those
caused during laser ablation and due to instrumental discrimination, is corrected using external zircon
standards. Total uncertainty for each laser analysis of an unknown is combined quadratically from the
uncertainty in the measured isotope ratios of the unknown and the uncertainty in the fractionation factors
calculated from the measurement of standards. For individual analyses we estimate that the accuracy and
precision are better than 4% at the 2 sigma level, with the largest contribution in uncertainty from the
measurement of the standards. Accuracy of age determinations in this study is on the order of 1% on the
basis of comparing the weighted average of the LA-ICP-MS determinations to the TIMS ages. Due to
unresolved contributions to uncertainty from the lack of a common Pb correction and from potential matrix
effects between standards and unknowns, however, this estimate cannot be universally applied to all
unknowns. Nevertheless, the results of this study provide an example of the type of precision and accuracy
that may be possible with this technique under ideal conditions. In summary, the laser ablation technique,
using a magnetic sector ICP-MS, can be used for the U-Pb dating of zircons with a wide range of ages and
is a useful complement to the established TIMS and SHRIMP techniques. This technique is especially well
suited to reconnaissance geochronologic and detrital zircon studies." name="DC.description" />
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    <h1 class="ep_tm_pagetitle">U-Pb dating of zircon by LA-ICP-MS</h1>
    <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Chang, Z.</span> and <span class="person_name">Vervoort, J. D.</span> and <span class="person_name">McClelland, W. C.</span> and <span class="person_name">Knaack, C.</span> (2006) <xhtml:em>U-Pb dating of zircon by LA-ICP-MS.</xhtml:em> Geochemistry Geophysics Geosystems, 7 (5). ISSN 1525-2027</p><p style="margin-bottom: 1em" class="not_ep_block"></p><table style="margin-bottom: 1em" class="not_ep_block"><tr><td valign="top" style="text-align:center"><a href="http://eprints.utas.edu.au/693/1/Chang_et_al.%2C_GGG%2C_2006.pdf"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" class="ep_doc_icon" border="0" /></a></td><td valign="top"><a href="http://eprints.utas.edu.au/693/1/Chang_et_al.%2C_GGG%2C_2006.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />701Kb</td><td><form method="get" accept-charset="utf-8" action="http://eprints.utas.edu.au/cgi/request_doc"><input accept-charset="utf-8" value="705" name="docid" type="hidden" /><div class=""><input value="Request a copy" name="_action_null" class="ep_form_action_button" onclick="return EPJS_button_pushed( '_action_null' )" type="submit" /> </div></form></td></tr></table><p style="margin-bottom: 1em" class="not_ep_block">Official URL: <a href="http://dx.doi.org/10.1029/2005GC001100">http://dx.doi.org/10.1029/2005GC001100</a></p><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">In this study we used LA-ICP-MS (laser ablation-inductively coupled plasma-mass spectrometry) to&#13;
determine U-Pb ages of 5 zircon samples of known age (1800 Ma to 50 Ma) in order to determine the&#13;
reproducibility, precision, and accuracy of this geochronologic technique. This work was performed using&#13;
a ThermoFinnigan Element2 magnetic sector double-focusing ICP-MS coupled with a New Wave&#13;
Research UP-213 laser system. The laser ablation pit sizes ranged from 30 to 40 mm in diameter. Laserinduced&#13;
time-dependent fractionation is corrected by normalizing measured ratios in both standards and&#13;
samples to the beginning of the analysis using the intercept method. Static fractionation, including those&#13;
caused during laser ablation and due to instrumental discrimination, is corrected using external zircon&#13;
standards. Total uncertainty for each laser analysis of an unknown is combined quadratically from the&#13;
uncertainty in the measured isotope ratios of the unknown and the uncertainty in the fractionation factors&#13;
calculated from the measurement of standards. For individual analyses we estimate that the accuracy and&#13;
precision are better than 4% at the 2 sigma level, with the largest contribution in uncertainty from the&#13;
measurement of the standards. Accuracy of age determinations in this study is on the order of 1% on the&#13;
basis of comparing the weighted average of the LA-ICP-MS determinations to the TIMS ages. Due to&#13;
unresolved contributions to uncertainty from the lack of a common Pb correction and from potential matrix&#13;
effects between standards and unknowns, however, this estimate cannot be universally applied to all&#13;
unknowns. Nevertheless, the results of this study provide an example of the type of precision and accuracy&#13;
that may be possible with this technique under ideal conditions. In summary, the laser ablation technique,&#13;
using a magnetic sector ICP-MS, can be used for the U-Pb dating of zircons with a wide range of ages and&#13;
is a useful complement to the established TIMS and SHRIMP techniques. This technique is especially well&#13;
suited to reconnaissance geochronologic and detrital zircon studies.</p></div><table style="margin-bottom: 1em" cellpadding="3" class="not_ep_block" border="0"><tr><th valign="top" class="ep_row">Item Type:</th><td valign="top" class="ep_row">Article</td></tr><tr><th valign="top" class="ep_row">Additional Information:</th><td valign="top" class="ep_row">http://www.agu.org/pubs/crossref/2006/2005GC001100.shtml</td></tr><tr><th valign="top" class="ep_row">Keywords:</th><td valign="top" class="ep_row">laser ablation; magnetic sector ICP-MS; U-Pb dating; zircon dating.</td></tr><tr><th valign="top" class="ep_row">Subjects:</th><td valign="top" class="ep_row"><a href="http://eprints.utas.edu.au/view/subjects/260100.html">260000 Earth Sciences &gt; 260100 Geology</a></td></tr><tr><th valign="top" class="ep_row">Collections:</th><td valign="top" class="ep_row">UNSPECIFIED</td></tr><tr><th valign="top" class="ep_row">ID Code:</th><td valign="top" class="ep_row">693</td></tr><tr><th valign="top" class="ep_row">Deposited By:</th><td valign="top" class="ep_row"><span class="ep_name_citation"><span class="person_name">Mr Ruben Chan</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">08 Feb 2007</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">31 Jan 2008 13:41</td></tr><tr><th valign="top" class="ep_row">ePrint Statistics:</th><td valign="top" class="ep_row"><a target="ePrintStats" href="/es/index.php?action=show_detail_eprint;id=693;">View statistics for this ePrint</a></td></tr></table><p align="right">Repository Staff Only: <a href="http://eprints.utas.edu.au/cgi/users/home?screen=EPrint::View&amp;eprintid=693">item control page</a></p>
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