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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.1986.050.356.04</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Petrology</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Eclogitic Amphibolites from the Grampian Moines</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Baker</surname>
<given-names>A. J.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">*</xref>
<aff>Department of Earth Sciences, Oxford University, Parks Road, Oxford OX1 3PR</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>*</label><p>Present address: Grant Institute of Geology, West Mains Road, Edinburgh EH9 3JW.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>6</month>
<year>1986</year>
</pub-date>
<volume>50</volume>
<issue>356</issue>
<fpage>217</fpage>
<lpage>221</lpage>
<history>
<date date-type="received">
<day>9</day>
<month>5</month>
<year>1985</year>
</date>
<date date-type="rev-recd">
<day>26</day>
<month>11</month>
<year>1985</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1986, The Mineralogical Society</copyright-statement>
<copyright-year>1986</copyright-year>
<abstract>
<title>Abstract</title>
<p>Amphibolites from the Grampian Moines of Scotland contain clinopyroxene-plagioclase symplectites and plagioclase-hornblende coronas around garnet. The clinopyroxene-plagioclase symplectites are interpreted as former omphacites. It is inferred that an eclogitic garnetomphacite-quartz assemblage once existed, but has since undergone partial reaction to an amphibolite facies hornblende-plagioclase assemblage. An early high-pressure metamorphic event occurred in parts of the Moine.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>amphibolites</kwd>
<kwd>eclogites</kwd>
<kwd>symplectites</kwd>
<kwd>coronas</kwd>
<kwd>Moines</kwd>
<kwd>Grampian Mountains</kwd>
</kwd-group>
</article-meta>
</front>
</article>
