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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.1985.049.354.09</article-id>
<title-group>
<article-title>Potassium Pargasite from Einst&#x00F6;dingen, L&#x00FC;tzow-Holm Bay, East Antarctica</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Matsubara</surname>
<given-names>S.</given-names>
</name>
<aff>Department of Geology, National Science Museum, 3-23-1 Hyakunin-cho, Shinjuku, Tokyo 160, Japan</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Motoyoshi</surname>
<given-names>Y.</given-names>
</name>
<aff>Department of Geology and Mineralogy, Faculty of Science, Hokkaido University, Kita-10, Nishi-8, Sapporo 060, Japan</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1985</year>
</pub-date>
<volume>49</volume>
<issue>354</issue>
<fpage>703</fpage>
<lpage>707</lpage>
<history>
<date date-type="received">
<day>4</day>
<month>12</month>
<year>1984</year>
</date>
<date date-type="rev-recd">
<day>20</day>
<month>2</month>
<year>1985</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1985, The Mineralogical Society</copyright-statement>
<copyright-year>1985</copyright-year>
<abstract>
<title>Abstract</title>
<p>Potassium pargasite containing 3.19 wt. % K<sub>2</sub>O was found in a skarn from the islet of Einst&#x00F6;dingen, L&#x00FC;tzow-Holm Bay, East Antarctica, together with some high potassium pargasitic amphiboles. A positive correlation is shown between Fe<sup>2+</sup>/(Mg+Fe<sup>2+</sup>) and K/(K + Na(<italic>A</italic>)) ratios in pargasitic amphiboles suggesting that the increase of Fe<sup>2+</sup> serve to stabilize high-K pargasites under the metamorphic conditions of the granulite facies.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>amphiboles</kwd>
<kwd>pargasite</kwd>
<kwd>Einst&#x00F6;dingen</kwd>
<kwd>Antarctica</kwd>
</kwd-group>
</article-meta>
</front>
</article>
