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<article article-type="other">
<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.1997.061.406.05</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Single Crystal Galena Pillars as Highly Anisometric Dissolution Forms</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Bonev</surname>
<given-names>Ivan K.</given-names>
</name>
<aff>Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Rice</surname>
<given-names>Clive M.</given-names>
</name>
<aff>Department of Geology &#x0026; Petroleum Geology, University of Aberdeen, Meston Building, Kings College, Aberdeen AB24 3UE, UK</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1997</year>
</pub-date>
<volume>61</volume>
<issue>406</issue>
<fpage>377</fpage>
<lpage>386</lpage>
<history>
<date date-type="received">
<day>5</day>
<month>8</month>
<year>1996</year>
</date>
<date date-type="rev-recd">
<day>1</day>
<month>10</month>
<year>1996</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1997, The Mineralogical Society</copyright-statement>
<copyright-year>1997</copyright-year>
<abstract>
<title>Abstract</title>
<p>Remarkable single crystal galena formations in the unique form of cylindrical or steep conical &#x2018;pillars&#x2019; with &#x2018;capitals&#x2019; of small rhombododecahedral single crystals of sphalerite, are described. It is suggested that the pillars result from a highly specific process of anisotropic mineral dissolution controlled by a system of internal channels in the original skeletal crystals and represent a kind of dissolution whiskers.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>galena</kwd>
<kwd>crystal morphology</kwd>
<kwd>dissolution</kwd>
<kwd>whiskers</kwd>
</kwd-group>
</article-meta>
</front>
</article>
