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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>C. J. Janik</dc:contributor>
  <dc:contributor>H. Delgado</dc:contributor>
  <dc:contributor>C. Werner</dc:contributor>
  <dc:contributor>D. Counce</dc:contributor>
  <dc:contributor>J.A. Stimac</dc:contributor>
  <dc:contributor>C. Siebe</dc:contributor>
  <dc:contributor>S.P. Love</dc:contributor>
  <dc:contributor>S.N. Williams</dc:contributor>
  <dc:contributor>T. Fischer</dc:contributor>
  <dc:contributor>L. Johnson</dc:contributor>
  <dc:creator>F. Goff</dc:creator>
  <dc:date>1998</dc:date>
  <dc:description>&lt;div id="15009100" class="article-section-wrapper js-article-section js-content-section  " data-section-parent-id="0"&gt;&lt;p&gt;Surveillance of Popocatépetl volcanic plume geochemistry and SO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;flux began in early 1994 after fumarolic and seismic activity increased significantly during 1993. Volatile traps placed around the summit were collected at near-monthly intervals until the volcano erupted on December 21, 1994. Additional trap samples were obtained in early 1996 before the volcano erupted again, emplacing a small dacite dome in the summit crater. Abundances of volatile constituents (ppm/day of Cl, S&lt;sub&gt;total&lt;/sub&gt;, F, CO&lt;sub&gt;2&lt;/sub&gt;, Hg, and As) varied, but most constituents were relatively high in early and late 1994. However, ratios of these constituents to Cl were highest in mid-1994. δ&lt;sup&gt;34&lt;/sup&gt;S-S&lt;sub&gt;total&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;in trap solutions ranged from 1.5‰ to 6.4‰; lowest values generally occurred during late 1994. δ&lt;sup&gt;13&lt;/sup&gt;C-CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;of trap solutions were greatly contaminated with atmospheric CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;and affected by absorption kinetics. When trap data are combined with SO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;flux measurements made through November 1996, Popocatépetl released about 3.9 Mt SO&lt;sub&gt;2&lt;/sub&gt;, 16 Mt CO&lt;sub&gt;2&lt;/sub&gt;, 0.75 Mt HCl, 0.075 Mt HF, 260 t As, 2.6 t Hg, and roughly 200 Mt H&lt;sub&gt;2&lt;/sub&gt;O. Near-vent gas concentrations in the volcanic plume measured by correlation spectrometer (COSPEC) and Fourier transform infrared (FTIR) commonly exceed human recommended exposure limits and may constitute a potential health hazard. Volatile geochemistry combined with petrologic observations and melt-inclusion studies show that mafic magma injection into a preexisting silicic chamber has accompanied renewed volcanism at Popocatépetl. Minor assimilation of Cretaceous wall rocks probably occurred in mid-1994.&lt;/p&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/0016-7606(1998)110&lt;0695:GSOMVA&gt;2.3.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Geological Society of America</dc:publisher>
  <dc:title>Geochemical surveillance of magmatic volatiles at Popocatepetl volcano, Mexico</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>