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<!DOCTYPE article SYSTEM "journalpublishing.dtd">
<article article-type="research-article">
<front>
<journal-meta>
<journal-id journal-id-type="archive">gsminmag</journal-id>
<journal-title>Mineralogical Magazine</journal-title>
<abbrev-journal-title abbrev-type="full">Mineralogical Magazine</abbrev-journal-title>
<issn pub-type="ppub">0026-461X</issn>
<publisher>
<publisher-name>Mineralogical Society</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1180/minmag.1980.043.332.02</article-id>
<title-group>
<article-title>An Evaluation of the Performance of an Inductively Coupled Plasma Source Spectrometer for the Determination of the Major and Trace Constituents of Silicate Rocks and Minerals</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Walsh</surname>
<given-names>J. N.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Howie</surname>
<given-names>R. A.</given-names>
</name></contrib>
<aff>Department of Geology, King's College, Strand, London WC2R 2LS</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1980</year>
</pub-date>
<volume>43</volume>
<issue>332</issue>
<fpage>967</fpage>
<lpage>974</lpage>
<history>
<date date-type="received">
<day>5</day>
<month>2</month>
<year>1980</year>
</date>
<date date-type="rev-recd">
<day>28</day>
<month>5</month>
<year>1980</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1980, The Mineralogical Society</copyright-statement>
<copyright-year>1980</copyright-year>
<abstract>
<title>Summary</title>
<p>The results of a study on the suitability of the inductively coupled plasma source spectrometer for the analysis of rocks and minerals are presented. The preparation of a stable solution of the elements to be measured is a prerequisite, and methods of sample preparation are described. It is shown that it is possible to measure all the major elements (excluding H<sub>2</sub>O and Fe<sup>2+</sup>) with acceptable precision and accuracy, and a wide range of trace elements down to the ppm level in the rock or mineral. Excluding sample preparation time, analysis and print-out of results as percent or ppm requires 1&#x2013;2 minutes for complete analysis. Data on possible interferences (spectral line overlap etc.) are presented and, using some analyses of rocks and minerals comparisons are made with other analytical methods.</p></abstract>
</article-meta>
</front>
</article>
