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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.1935.024.149.03</article-id>
<title-group>
<article-title>Ankerites of the Northumberland Coal-Field</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hawkes</surname>
<given-names>L.</given-names>
</name><degrees>D.Sc., F.G.S.</degrees>
<aff>Reader in Geology, Bedford College, University of London</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Smythe</surname>
<given-names>J. A.</given-names>
</name><degrees>Ph.D., D.Sc.</degrees>
<aff>Lecturer in Metallurgy, Armstrong College, Newcastle-on-Tyne.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1935</year>
</pub-date>
<volume>24</volume>
<issue>149</issue>
<fpage>65</fpage>
<lpage>75</lpage>
<copyright-statement>Copyright &#x00A9; 1935, The Mineralogical Society</copyright-statement>
<copyright-year>1935</copyright-year>
<abstract>
<title>Summary</title>
<p>1. Ankerite and ankeritic calcite are described from veins in the Coal Measures on the coast at Hartley and from various seams in the Northumberland coal-field. Evidence is given that, in the portion of the coal-field examined, both minerals are of constant composition, and that the deposition of the ankerite preceded that of the ankeritic calcite.</p>
<p>2. The ankerites are members of an isomorphous series consisting of dolomite MgCO<sub>3</sub>.CaCO<sub>3</sub> and ferrodolomite FeCO<sub>3</sub>.CaCO<sub>3</sub>, with small amounts of mangandolomite MnCO<sub>3</sub>.CaCO<sub>3</sub>, and they may hold up to 20 % of CaCO<sub>3</sub> a in solid solution.</p>
<p>3. The refractive indices (ordinary ray) of the ankerites are examined, and the value deduced for FeCO<sub>3</sub>.CaCO<sub>3</sub> is 1&#x2022;765.</p></abstract>
</article-meta>
</front>
</article>
