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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.1987.051.362.11</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Evidence for Differences in Growth Rate Among Garnets in Pelitic Schists from Northern Sutherland, Scotland</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Finlay</surname>
<given-names>C. A.</given-names>
</name>
<aff>Pollution Control Group, Department of Chemical Engineering, University of Natal, King George V Avenue, Durban 4001, South Africa</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Kerr</surname>
<given-names>A.</given-names>
</name>
<aff>Department of Geology and Applied Geology, University of Natal, King George V Avenue, Durban 4001, South Africa</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>10</month>
<year>1987</year>
</pub-date>
<volume>51</volume>
<issue>62</issue>
<fpage>569</fpage>
<lpage>576</lpage>
<history>
<date date-type="received">
<day>13</day>
<month>1</month>
<year>1986</year>
</date>
<date date-type="rev-recd">
<day>8</day>
<month>8</month>
<year>1986</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1987, The Mineralogical Society</copyright-statement>
<copyright-year>1987</copyright-year>
<abstract>
<title>Abstract</title>
<p>MnO zoning profiles for various sizes of garnets from two pelitic schists were examined. The data from garnets of specimen A are consistent with a constant growth law, while the compositional-crystal size relationships of garnets from specimen B are best explained by heterogeneous growth rates.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>garnet</kwd>
<kwd>growth rate</kwd>
<kwd>pelitic schists</kwd>
<kwd>Sutherland</kwd>
<kwd>Scotland</kwd>
</kwd-group>
</article-meta>
</front>
</article>
