<?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.1980.043.331.14</article-id>
<title-group>
<article-title>Changes in the Crystal Morphology of Synthetic Reedmergnerite (NaBSi<sub>3</sub>O<sub>8</sub>) During Ordering Experiments</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Mason</surname>
<given-names>R. A.</given-names>
</name>
<aff>Dept. of Geology, The University, Manchester M13 9PL, Great Britain*</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN"><label>*</label><p>Present address: The University of Chicago, Dept. of the Geophysical Sciences, 5734 S. Ellis Avenue, Chicago, Illinois 60637, USA.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>9</month>
<year>1980</year>
</pub-date>
<volume>43</volume>
<issue>331</issue>
<fpage>905</fpage>
<lpage>908</lpage>
<history>
<date date-type="received">
<day>15</day>
<month>1</month>
<year>1980</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1980, The Mineralogical Society</copyright-statement>
<copyright-year>1980</copyright-year>
<abstract>
<title>Summary</title>
<p>The morphologies of hydrothermally grown reedmergnerite crystals change systematically with time and rate of change of B, Si order. Three stages in this process are recognized: (1) Growth of well-faceted crystals. (2) Development of etching leading to the formation of irregular grains. (3) Modification of irregular grains to form rounded or ellipsoidal crystals. A solutionreprecipitation process is responsible for the morphological changes and the increase in degree of order of B and Si with time at constant temperature and pressure.</p></abstract>
</article-meta>
</front>
</article>
