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<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.1960.032.251.02</article-id>
<title-group>
<article-title>The Amygdale Minerals in the Tertiary Lavas of Ireland. IV. The Crystal Habit of Calcite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Walker</surname>
<given-names>G. P. L</given-names>
</name><degrees>M.Sc., Ph.D., F.G.S.</degrees>
<aff>Dept. of Geology, Imperial College, London S.W. 7</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1960</year>
</pub-date>
<volume>32</volume>
<issue>251</issue>
<fpage>609</fpage>
<lpage>618</lpage>
<copyright-statement>Copyright &#x00A9; 1960, The Mineralogical Society</copyright-statement>
<copyright-year>1960</copyright-year>
<abstract>
<title>Summary</title>
<p>Calcite is widespread in amygdales associated with the zeolites; the characteristic forms being &#x007B;<inline-formula><mml:math><mml:mrow><mml:mn>0</mml:mn><mml:mn>2</mml:mn><mml:mover><mml:mi>2</mml:mi><mml:mo>&#x00AF;</mml:mo></mml:mover></mml:mrow><mml:mn>1</mml:mn></mml:math></inline-formula>&#x007D; and a steep scalenohedron in the zone [<inline-formula><mml:math><mml:mrow><mml:mover><mml:mn>1</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>101</mml:mn></mml:mrow></mml:math></inline-formula>], usually &#x007B;<inline-formula><mml:math><mml:mrow><mml:mn>13.11.</mml:mn><mml:mover><mml:mn>24</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>.2</mml:mn></mml:mrow></mml:math></inline-formula>&#x007D;. Crystals from one locality have faces of &#x007B;<inline-formula><mml:math><mml:mrow><mml:mn>16.1.</mml:mn><mml:mover><mml:mn>17</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>.0</mml:mn></mml:mrow></mml:math></inline-formula>&#x007D;, a form new to calcite.</p></abstract>
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