<?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:creator>L. Paul Greenland</dc:creator>
  <dc:date>1973</dc:date>
  <dc:description>&lt;div id="aep-abstract-id4" class="abstract author"&gt;&lt;div id="aep-abstract-sec-id5"&gt;&lt;p id="simple-para.0010"&gt;Rocks containing 10–140 ng of indium per g are decomposed with hydrofluoric and nitric acids in the presence of&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;114&lt;/sup&gt;In. Indium is separated from other constituents by sequential extractions of the bromide, cupferronate, and acetylacetonate, and is then reacted with a substoichiometric amont of EDTA. Excess of indium is removed by acetylacetone extraction and the specific activity of the complexed fraction is determined by counting&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;114&lt;/sup&gt;In. Analyses of the U.S.G.S. standard rocks are reported. These show good agreement with previous neutron activation analyses. Repetitive rock analyses indicated an analytical precision of ±4–7%.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/S0003-2670(01)80230-0</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevierr</dc:publisher>
  <dc:title>Determination of indium in rocks by substoichiometric radioisotope dilution analysis</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>