<?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>E.Y. Campbell</dc:contributor>
  <dc:contributor>P. J. Aruscavage</dc:contributor>
  <dc:creator>F.O. Simon</dc:creator>
  <dc:date>1977</dc:date>
  <dc:description>&lt;p&gt;Thallium was determined in 16 USGS standard rocks by atomic absorption spectroscopy in which a heated graphite atomizer was used after extraction as thallium iodide into amyl acetate. Four subsamples from four bottles of each standard sample, except G-1 and W-1, were analyzed in random order, and the average thallium contents in parts per million (as Tl) were AGV-1, 0.41; GSP-1, 1.63; G-2, 1.08; BCR-1, 0.35; SDC-1, 0.80; MAG-1, 0.79; BHVO-1, 0.049; SCO-1, 0.79; SGR-1, 0.34; QLO-1, 0.23; RGM-1, 1.07 ; STM-1, 0.30; DTS-1, &amp;lt;0.005; and PCC-1, &amp;lt;0.005. The analysis of variance showed that all samples may be considered homogeneous at &lt;i&gt;F&lt;/i&gt;&lt;sub&gt;0.975&lt;/sub&gt;&amp;nbsp;and only GSP-1 may be considered heterogeneous at &lt;i&gt;F&lt;/i&gt;&lt;sub&gt;0.95&lt;/sub&gt;. The Tl contents of G-1 and W-1 are 1.0 and 0.12 ppm, respectively.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Thallium contents of 16 USGS standard rocks</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>