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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.1973.039.304.08</article-id>
<title-group>
<article-title>Hydrothermal Synthesis of Albite: The Effect of NaOH on Obliquity</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Trembath</surname>
<given-names>L. T.</given-names>
</name>
<aff>Dept. of Geology, University of New Brunswick, Fredericton, New Brunswick, Canada</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1973</year>
</pub-date>
<volume>39</volume>
<issue>304</issue>
<fpage>455</fpage>
<lpage>463</lpage>
<history>
<date date-type="received">
<day>12</day>
<month>1</month>
<year>1973</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1973, The Mineralogical Society</copyright-statement>
<copyright-year>1973</copyright-year>
<abstract>
<title>Summary</title>
<p>A series of albites was synthesized in the presence of aqueous NaOH fluids (concentration 0 to 4N NaOH, <italic>P</italic><sub>fluid</sub> = 15000 1b/in<sup>2</sup>) over the temperature range 300 to 500 &#x00B0;C. At fixed temperature-pressure conditions increasing NaOH concentration of the initial fluid can be correlated with decreasing obliquity of the albites.</p></abstract>
</article-meta>
</front>
</article>
