<?xml version="1.0"?>
<!DOCTYPE article SYSTEM "journalpublishing.dtd">
<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.1989.053.370.05</article-id>
<title-group>
<article-title>Studies of the Orthoamphiboles. IV. M&#x00F6;ssbauer Spectra of Anthophyllites and Gedrites</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Law</surname>
<given-names>Anthony D.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">*</xref>
<aff>Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX13PR</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>*</label><p>Present address: BP Exploration Company Ltd., Britannic House, Moor Lane, London EC2Y 9BU.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>4</month>
<year>1989</year>
</pub-date>
<volume>53</volume>
<issue>370</issue>
<fpage>181</fpage>
<lpage>191</lpage>
<history>
<date date-type="received">
<day>12</day>
<month>4</month>
<year>1988</year>
</date>
<date date-type="rev-recd">
<day>15</day>
<month>11</month>
<year>1988</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1989, The Mineralogical Society</copyright-statement>
<copyright-year>1989</copyright-year>
<abstract>
<title>Abstract</title>
<p>Fitted M&#x00F6;ssbauer spectra are presented for a set of anthophyllites and gedrites. Despite their complexity it is possible to obtain fits for gedrite spectra and the M&#x00F6;ssbauer parameters are consistent with results for anthophyllites from this and previous studies. At least three doublets are required to fit the Fe<sup>2+</sup> absorption in gedrites; there is no single model at present to explain the behaviour of the spectra. Fe<sup>3+</sup> absorption is also resolved.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>orthoamphiboles</kwd>
<kwd>M&#x00F6;ssbauer spectra</kwd>
<kwd>anthophyllites</kwd>
<kwd>gedrites</kwd>
</kwd-group>
</article-meta>
</front>
</article>
