<?xml version="1.0"?>
<!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.1956.031.232.06</article-id>
<title-group>
<article-title>On the Correlation of Physical Properties with Chemical Composition in Multivariate Systems</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hey</surname>
<given-names>Max H.</given-names></name> <degrees>H.A., D.Sc.</degrees>
<aff>Department of Mineralogy, British Museum (Natural History)</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1956</year>
</pub-date>
<volume>31</volume>
<issue>232</issue>
<fpage>69</fpage>
<lpage>95</lpage>
<copyright-statement>Copyright &#x00A9; 1956, The Mineralogical Society</copyright-statement>
<copyright-year>1956</copyright-year>
<abstract>
<title>Summary</title>
<p>A systematic and time-saving procedure for the correlation of optical or other physical properties with chemical composition is outlined, and is applicable even where the composition is complex and involves several variables. The procedure is applied to anthophyllite, for which the following partial regression equations are derived:</p>
<p><italic>&#x03B3;</italic> = 1&#x00B7;7249&#x2212;0&#x00B7;0130Si+0&#x00B7;0140(Ti+Fe&#x2034;+Fe&#x2032;+Mn)&#x00B1;0&#x00B7;0012,</p>
<p><italic>&#x03B2;</italic> = 1&#x00B7;7275&#x2212;0&#x00B7;0142Si+0&#x00B7;024(Ti+Fe&#x2034;)+0&#x00B7;0110(Fe&#x2033;+Mn)&#x00B1;0&#x00B7;0015,</p>
<p><italic>&#x03B1;</italic> = 1&#x00B7;6951&#x2212;0&#x00B7;0117Si+0&#x00B7;040(Ti+Fe&#x2034;)+0&#x00B7;0133(Fe&#x2033;+Mn)&#x00B1;0&#x00B7;0025, p <italic>b</italic>(&#x00C5;.) = 16&#x00B7;44+0&#x00B7;28Si&#x2212;0&#x00B7;13Mg+0&#x00B7;40(Ca+Na+K)&#x00B1;0&#x00B7;04.</p>
<p>The <italic>a</italic> and <italic>c</italic> cell-dimensions appear to be constant, within the experimental error of the available data.</p></abstract>
</article-meta>
</front>
</article>
