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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.1983.047.343.04</article-id>
<title-group>
<article-title>Chemical Distinction Between Igneous and Metamorphic Orthopyroxenes Especially Those Coexisting with Ca-rich Clinopyroxenes: A Re-Evaluation</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Rietmeijer</surname>
<given-names>Frans J. M.</given-names>
</name>
<aff>Department of Petrology, Instituut voor Aardwetenschappen, Budapestlaan 4, 3584 CD Utrecht, The Netherlands</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1983</year>
</pub-date>
<volume>47</volume>
<issue>343</issue>
<fpage>143</fpage>
<lpage>151</lpage>
<history>
<date date-type="received">
<day>15</day>
<month>5</month>
<year>1981</year>
</date>
<date date-type="rev-recd">
<day>1</day>
<month>10</month>
<year>1982</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1983, The Mineralogical Society</copyright-statement>
<copyright-year>1983</copyright-year>
<abstract>
<title>Abstract</title>
<p>A previously suggested simple relationship in a diagram of(Al<sub>2</sub>O<sub>3</sub> <italic>vs.</italic> MgO + FeO + Fe<sub>2</sub>O<sub>3</sub>)<sub>opx</sub> for the distinction between igneous and metamorphic orthopyroxenes is shown to be inadequate. A revised diagram is presented and its limitations are discussed. A diagram showing Fe<sup>2+</sup>/(Fe<sup>2+</sup> + Mg) <italic>vs.</italic> 100Ca/(Fe<sup>2+</sup> + Mg + Ca) for orthopyroxenes coexisting with Ca-rich clinopyroxenes proves to be useful for the discrimination of igneous and metamorphic orthopyroxenes and for evaluation of the extent and physical conditions of regional orthopyroxene re-equilibration.</p></abstract>
</article-meta>
</front>
</article>
