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<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.1964.033.266.03</article-id>
<title-group>
<article-title>The Lattice Parameters of High-Temperature Triclinic Sodic Feldspars</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Carmichael</surname>
<given-names>I. S. E.</given-names>
</name><degrees>M.A., Ph.D.</degrees>
<xref ref-type="author-notes" rid="FN1">1</xref>
<aff>Department of Geology, Imperial College of Science London, S.W. 7</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Mackenzie</surname>
<given-names>W. S.</given-names>
</name><degrees>M.A., B.Sc., Ph.D., F.R.S.E.</degrees>
<aff>Department of Geology, The University, Manchester, 13</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>1</label><p>Present address: Dept. of Geology and Geophysics, Univ. of California, Berkeley.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>9</month>
<year>1964</year>
</pub-date>
<volume>33</volume>
<issue>266</issue>
<fpage>949</fpage>
<lpage>962</lpage>
<copyright-statement>Copyright &#x00A9; 1964, The Mineralogical Society</copyright-statement>
<copyright-year>1964</copyright-year>
<abstract>
<title>Summary</title>
<p>The lattice parameters of twenty calcium-bearing anorthoclases and potassium-bearing acid plagioclases have been determined by powder methods. The <inline-formula><mml:math><mml:mrow><mml:mn>20</mml:mn><mml:mover><mml:mn>1</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover></mml:mrow></mml:math></inline-formula> spacing of the homogenized anorthoclases gives a good measure of the Or content irrespective of the amount of calcium present ; this spacing combined with <italic>&#x03B1;</italic>* (010): (001) may be used to determine the ternary composition of homogeneous feldspars more potassic than approximately Or<sub>15</sub>. The lattice parameters of feldspars less potassic than Or<sub>15</sub> cannot be used for the determination of their ternary composition.</p></abstract>
</article-meta>
</front>
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