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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.1959.032.246.07</article-id>
<title-group>
<article-title>A New Method for Orthoscopic Adjustment with the Fedorov stage</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hallimond</surname>
<given-names>A. F.</given-names>
</name><degrees>M.A., Sc. D.</degrees>
<aff>75 Corringham Road, London, N.W. 11</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1959</year>
</pub-date>
<volume>32</volume>
<issue>246</issue>
<fpage>245</fpage>
<lpage>250</lpage>
<copyright-statement>Copyright &#x00A9; 1959, The Mineralogical Society</copyright-statement>
<copyright-year>1959</copyright-year>
<abstract>
<title>Summary</title>
<p>A new method is described to replace the standard procedure for completing the adjustment of an optical symmetry plane, with conditions for the accurate use of the biquartz. Extinction measurements are plotted to show the wide range of sensitivity (for the adjustment of A<sub>1</sub> and A<sub>2</sub>) at various directions in the symmetry planes of a plagioclase. It is proposed that A<sub>1</sub> and A<sub>2</sub>should be adjusted at different settings of A<sub>4</sub> so as to obtain maximum sensitivity for each of those axes.</p></abstract>
</article-meta>
</front>
</article>
