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<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.1983.047.344.13</article-id>
<title-group>
<article-title>New IR and XRD Data for Leadhillite of Ideal Composition</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Russell</surname>
<given-names>J. D.</given-names>
</name>
<aff>Macaulay Institute for Soil Research, Craigiebuckler, Aberdeen AB9 2QJ</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Milodowski</surname>
<given-names>A. E.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">*</xref>
<aff>Department of Geology, King&#x2019;s College, Strand, London WC2R 2LS</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Fraser</surname>
<given-names>A. R.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Clark</surname>
<given-names>D. R.</given-names>
</name></contrib>
<aff>Macaulay Institute for Soil Research, Craigiebuckler, Aberdeen AB9 2QJ</aff></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>*</label><p>Present address: IGS Environmental Protection Unit, Bldg 151, Harwell Laboratory, Oxfordshire OXll 0RA.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>9</month>
<year>1983</year>
</pub-date>
<volume>47</volume>
<issue>344</issue>
<fpage>371</fpage>
<lpage>375</lpage>
<history>
<date date-type="received">
<day>8</day>
<month>9</month>
<year>1982</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1983, The Mineralogical Society</copyright-statement>
<copyright-year>1983</copyright-year>
<abstract>
<title>Abstract</title>
<p>The infra-red spectrum and X-ray powder pattern of a chemically analysed specimen of leadhillite, a lead carbonate sulphate hydroxide mineral from Leadhills, Scotland, are shown to be different from those in the literature. The IR spectra of several specimens suggest that mutual replacement of SO<sub>4</sub>, CO<sub>3</sub>, and OH may occur in this mineral, and it is thought that this might be responsible for the observed variation in X-ray spacings.</p></abstract>
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