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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.1982.046.339.16</article-id>
<title-group>
<article-title>Chromian Mica from Sierra Nevada, Spain</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Mart&#x00ED;n-Rabios</surname>
<given-names>J. D.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Rodriguez-Gallego</surname>
<given-names>M.</given-names>
</name></contrib>
<aff>Department of Crystallography and Mineralogy, University of Granada, Spain</aff></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1982</year>
</pub-date>
<volume>46</volume>
<issue>339</issue>
<fpage>269</fpage>
<lpage>272</lpage>
<history>
<date date-type="received">
<day>2</day>
<month>12</month>
<year>1980</year>
</date>
<date date-type="rev-recd">
<day>23</day>
<month>6</month>
<year>1981</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1982, The Mineralogical Society</copyright-statement>
<copyright-year>1982</copyright-year>
<abstract>
<title>Synopsis</title>
<p><sc>Emerald</sc> green chromian 2<italic>M</italic><sub>1</sub> mica occurs in metamorphosed and metasomatized limestones, related to serpentinic rocks from Sierra Nevada, Spain. Chemical analysis gave: SiO<sub>2</sub> 44.51, Al<sub>2</sub>O<sub>3</sub> 27.60, TiO<sub>2</sub> 0.17, Cr<sub>2</sub>O<sub>3</sub> 3.35, Fe<sub>2</sub>O<sub>3</sub> 1.76, FeO 0.07, MnO 0.00, MgO 8.59, Li<sub>2</sub>O 0.03, Rb<sub>2</sub>O 0.01, BaO 0.01, CaO 1.71, Na<sub>2</sub>O 0.40, K<sub>2</sub>O 7.86, H<sub>2</sub>O 4.21 = 100.28. Optic properties are: pleochroism <italic>X</italic> blue, <italic>Y</italic> green, <italic>Z</italic> bluish green; refractive indices: <italic>&#x03B1;</italic>=1.562, <italic>&#x03B2;</italic>=1.611, <italic>&#x03B3;</italic>=1.616 (yellow light); inclined dispersion, r &#x003E; v. Orientation: second order mica. Refined parameters are <italic>a</italic> = 5.2116(6), <italic>b</italic> = 9.045(2), <italic>c</italic> = 19.97(2)&#x00C5;, <italic>&#x03B2;</italic> = 95.7(3)&#x00B0;. The structure is discussed and an order in the octahedral <italic>M</italic>(1) sites is observed, but no ordering in the tetrahedral <italic>T</italic>(1) and <italic>T</italic>(2) cations is detected. The mica described is a mariposite with anoma-lously high contents of Ca and Mg.</p></abstract>
</article-meta>
</front>
</article>
