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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.1994.058.393.08</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Absorption Coefficients of Overtone and Combination Modes of Quartz</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Shinoda</surname>
<given-names>Keiji</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Aikawa</surname>
<given-names>Nobuyuki</given-names>
</name></contrib>
<aff>Department of Geosciences, Faculty of Science, Osaka City University, Sugimoto 3-3-138, Sumiyoshi, Osaka 558, Japan</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1994</year>
</pub-date>
<volume>58</volume>
<issue>393</issue>
<fpage>601</fpage>
<lpage>606</lpage>
<history>
<date date-type="received">
<day>10</day>
<month>1</month>
<year>1994</year>
</date>
<date date-type="rev-recd">
<day>27</day>
<month>4</month>
<year>1994</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1994, The Mineralogical Society</copyright-statement>
<copyright-year>1994</copyright-year>
<abstract>
<title>Abstract</title>
<p>The <italic>a</italic>-, <italic>&#x03C3;</italic>- and &#x03C0;-spectra of quartz in the IR regions were measured under FTIR spectroscopy, and overtone and combination modes perpendicular to the <italic>c</italic>-axis of quartz were confirmed to be electric vector active by the coincidence of the <italic>a</italic>-spectrum with the <italic>&#x03C3;</italic>-spectrum among the three kinds of spectra. Absorption coefficients of overtone and combination modes intrinsic to the <italic>a- &#x03C3;-</italic>, and &#x043F;-spectra of quartz were measured. The thickness of quartz thin sections can be determined by applying the absorption coefficients obtained from the &#x03B1;- and &#x03C3;-spectra to the polarized IR absorption spectra measured under <italic>E</italic> &#x22A5; the <italic>c</italic>-axis.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>polarized absorbance spectrum</kwd>
<kwd>absorption coefficient</kwd>
<kwd>thickness determination</kwd>
<kwd>quartz</kwd>
</kwd-group>
</article-meta>
</front>
</article>
