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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.1985.049.350.13</article-id>
<title-group>
<article-title>The Structure of Junitoite, CaZn<sub>2</sub>Si<sub>2</sub>O<sub>7</sub>&#x00B7;H<sub>2</sub>O</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hamilton</surname>
<given-names>R. D.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Finney</surname>
<given-names>J. J.</given-names>
</name></contrib>
<aff>Department of Geology, Colorado School of Mines, Golden, Colorado 80401, USA</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1985</year>
</pub-date>
<volume>49</volume>
<issue>350</issue>
<fpage>91</fpage>
<lpage>95</lpage>
<history>
<date date-type="received">
<day>11</day>
<month>6</month>
<year>1984</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1985, The Mineralogical Society</copyright-statement>
<copyright-year>1985</copyright-year>
<abstract>
<title>Abstract</title>
<p>Junitoite, CaZn<sub>2</sub>Si<sub>2</sub>O<sub>7</sub>&#x00B7;H<sub>2</sub>O, is orthorhombic, space group <italic>Area</italic>2, with <italic>a</italic> = 12.510, <italic>b</italic> = 6.318, <italic>c</italic> = 8.561 &#x00C5;, Z = 4. The structure, determined on the basis of three-dimensional Mo-<italic>K&#x03B1;</italic> intensity data for 745 reflections refined to <italic>R</italic> = 0.10. The structure consists of ZnO<sub>4</sub> tetrahedral chains along <italic>b</italic> joined by Si<sub>2</sub>O<sub>4</sub> groups along <italic>a</italic> and <italic>c</italic> to form a three-dimensional network. Ca occurs in distorted CaO<sub>5</sub>(H<sub>2</sub>O) octahedra. The structure shows similarities to hemimorphite and Ca-Zn silicates but represents a unique tetrahedral framework.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>crystal structure</kwd>
<kwd>junitoite</kwd>
</kwd-group>
</article-meta>
</front>
</article>
