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<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.1966.035.275.07</article-id>
<title-group>
<article-title>A Simplified Method of 2 V Determination Using 3- and 4-Axis Stages</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Ehlers</surname>
<given-names>Ernest G.</given-names>
</name>
<aff>Department of Mineralogy, The Ohio State University, Columbus, Ohio</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1966</year>
</pub-date>
<volume>35</volume>
<issue>275</issue>
<fpage>958</fpage>
<lpage>962</lpage>
<history>
<date date-type="received">
<day>12</day>
<month>11</month>
<year>1965</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1966, The Mineralogical Society</copyright-statement>
<copyright-year>1966</copyright-year>
<abstract>
<title>Summary</title>
<p>A method is presented for use with a 3- or 4-axis stage whereby a biaxial mineral, after being oriented into the cardinal position by means of the inner vertical, NS., and EW. axes, can be placed into an orientation suitable for measurement of the 2 V as required by the Berek method. A table of the necessary manipulations is given. The stereographic projection is only used to determine rotational corrections.</p></abstract>
</article-meta>
</front>
</article>
