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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.1965.035.272.05</article-id>
<title-group>
<article-title>A Note on Varlamoffite and Associated Minerals from the Batang Padang District, Perak, Malaya, Malaysia<xref ref-type="fn" rid="FN1">1</xref></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Alexander,</surname>
<given-names>J. B.</given-names>
</name><degrees>C.B.E., Ph.D., F.G.S.</degrees>
<aff>Director Geological Survey, Malaya</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Flinter</surname>
<given-names>B. H.</given-names>
</name><degrees>B.Sc.</degrees>
<aff>Senior Geologist, Malaya</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="other" id="FN1"><label>1</label><p>Compiled from material included in a cyclostyled circular issued by the Director of the Geological Survey, Malaysia, for internal distribution.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>12</month>
<year>1965</year>
</pub-date>
<volume>35</volume>
<issue>272</issue>
<fpage>622</fpage>
<lpage>627</lpage>
<history>
<date date-type="received">
<day>21</day>
<month>4</month>
<year>1965</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1965, The Mineralogical Society</copyright-statement>
<copyright-year>1965</copyright-year>
<abstract>
<title>Summary</title>
<p>A new occurrence of varlamoffite is described, and the status of this species is considered; the term is best employed for cryptocrystalline yellowish material consisting predominantly of Sn and H<sub>2</sub>0 that may yield a diffuse powder pattern comparable to, or closely resembling that of cassiterite, but does yield a powder pattern identical with that of cassiterite after heat-treatment at about 1200&#x00B0; C. A new mineral, malayaite, CaSnSiO<sub>5</sub>, is briefly described; it is isostructural with sphene.</p></abstract>
</article-meta>
</front>
</article>
