<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Mauricio Ibanez-Mejia</dc:contributor>
  <dc:contributor>Seth D. Burgess</dc:contributor>
  <dc:contributor>Matthew A. Coble</dc:contributor>
  <dc:contributor>Umberto G Gordani</dc:contributor>
  <dc:contributor>Joel DesOrmeau</dc:contributor>
  <dc:contributor>George E. Gehrels</dc:contributor>
  <dc:contributor>Xianhua Li</dc:contributor>
  <dc:contributor>Scott MacLennan</dc:contributor>
  <dc:contributor>Mark Pecha</dc:contributor>
  <dc:contributor>Kei Sato</dc:contributor>
  <dc:contributor>Blair Schoene</dc:contributor>
  <dc:contributor>Victor A. Valencia</dc:contributor>
  <dc:contributor>Jeffrey D. Vervoort</dc:contributor>
  <dc:contributor>Tiantian Wang</dc:contributor>
  <dc:creator>Michael P Eddy</dc:creator>
  <dc:date>2019</dc:date>
  <dc:description>&lt;div class="abstract-group"&gt;&lt;div class="article-section__content en main"&gt;&lt;p&gt;We present multitechnique U-Pb geochronology and Hf isotopic data from zircon separated from rapakivi biotite granite within the Eocene Golden Horn batholith in Washington, USA. A weighted mean of twenty-five Th-corrected&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;206&lt;/sup&gt;Pb/&lt;sup&gt;238&lt;/sup&gt;U zircon dates produced at two independent laboratories using chemical abrasion-isotope dilution-thermal ionisation mass&amp;nbsp;spectrometry (CA-ID-TIMS) is 48.106&amp;nbsp;±&amp;nbsp;0.023&amp;nbsp;Ma (2&lt;i&gt;s&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;analytical including tracer uncertainties, MSWD&amp;nbsp;=&amp;nbsp;1.53) and is our recommended date for GHR1 zircon. Microbeam&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;206&lt;/sup&gt;Pb/&lt;sup&gt;238&lt;/sup&gt;U dates from laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) and secondary ion mass spectrometry (SIMS) laboratories are reproducible and in agreement with the CA-ID-TIMS date to within &amp;lt;&amp;nbsp;1.5%. Solution multi-collector ICP-MS (MC-ICP-MS) measurements of Hf isotopes from chemically purified aliquots of GHR1 yield a mean&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;176&lt;/sup&gt;Hf/&lt;sup&gt;177&lt;/sup&gt;Hf of 0.283050&amp;nbsp;±&amp;nbsp;17 (2&lt;i&gt;s&lt;/i&gt;,&lt;i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;n&amp;nbsp;&lt;/i&gt;=&lt;i&gt;&amp;nbsp;&lt;/i&gt;10), corresponding to a εHf&lt;sub&gt;0&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;of +9.3. Hafnium isotopic measurements from two LA-ICP-MS laboratories are in agreement with the solution MC-ICP-MS value. The reproducibility of&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;206&lt;/sup&gt;Pb/&lt;sup&gt;238&lt;/sup&gt;U and&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;176&lt;/sup&gt;Hf/&lt;sup&gt;177&lt;/sup&gt;Hf ratios from GHR1 zircon across a variety of measurement techniques demonstrates their homogeneity in most grains. Additionally, the effectively limitless reserves of GHR1 material from an accessible exposure suggest that GHR1 can provide a useful reference material for U-Pb geochronology of Cenozoic zircon and Hf isotopic measurements of zircon with radiogenic&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;176&lt;/sup&gt;Hf/&lt;sup&gt;177&lt;/sup&gt;Hf.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1111/ggr.12246</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley</dc:publisher>
  <dc:title>GHR1 Zircon – A new Eocene natural reference material for microbeam U-Pb geochronology and Hf isotopic analysis of zircon</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>