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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>Christophe Hemond</dc:contributor>
  <dc:contributor>Anne Briais</dc:contributor>
  <dc:contributor>Marcia Maia</dc:contributor>
  <dc:contributor>Daniel S. Scheirer</dc:contributor>
  <dc:contributor>Sharon L. Walker</dc:contributor>
  <dc:contributor>Tingting Wang</dc:contributor>
  <dc:contributor>Yongshun John Chen</dc:contributor>
  <dc:creator>Edward Baker</dc:creator>
  <dc:date>2014</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Multiple geological processes affect the distribution of hydrothermal venting along a mid-ocean ridge. Deciphering the role of a specific process is often frustrated by simultaneous changes in other influences. Here we take advantage of the almost constant spreading rate (65&amp;ndash;71 mm/yr) along 2500 km of the Southeast Indian Ridge (SEIR) between 77&amp;deg;E and 99&amp;deg;E to examine the spatial density of hydrothermal venting relative to regional and segment-scale changes in the apparent magmatic budget. We use 227 vertical profiles of light backscatter and (on 41 profiles) oxidation-reduction potential along 27 first and second-order ridge segments on and adjacent to the Amsterdam-St. Paul (ASP) Plateau to map&amp;nbsp;&lt;/span&gt;&lt;i&gt;p&lt;span&gt;h&lt;/span&gt;&lt;/i&gt;&lt;span&gt;, the fraction of casts detecting a plume. At the regional scale, venting on the five segments crossing the magma-thickened hot spot plateau is almost entirely suppressed (&lt;/span&gt;&lt;i&gt;p&lt;span&gt;h&lt;/span&gt;&lt;/i&gt;&lt;span&gt;&amp;thinsp;=&amp;thinsp;0.02). Conversely, the combined&amp;nbsp;&lt;/span&gt;&lt;i&gt;p&lt;span&gt;h&lt;/span&gt;&lt;/i&gt;&lt;span&gt;&amp;nbsp;(0.34) from all other segments follows the global trend of&amp;nbsp;&lt;/span&gt;&lt;i&gt;p&lt;span&gt;h&lt;/span&gt;&lt;/i&gt;&lt;span&gt;&amp;nbsp;versus spreading rate. Off the ASP Plateau, multisegment trends in&amp;nbsp;&lt;/span&gt;&lt;i&gt;p&lt;span&gt;h&lt;/span&gt;&lt;/i&gt;&lt;span&gt;&amp;nbsp;track trends in the regional axial depth, high where regional depth increases and low where it decreases. At the individual segment scale, a robust correlation between&amp;nbsp;&lt;/span&gt;&lt;i&gt;p&lt;span&gt;h&lt;/span&gt;&lt;/i&gt;&lt;span&gt;&amp;nbsp;and cross-axis inflation for first-order segments shows that different magmatic budgets among first-order segments are expressed as different levels of hydrothermal spatial density. This correlation is absent among second-order segments. Eighty-five percent of the plumes occur in eight clusters totaling &amp;sim;350 km. We hypothesize that these clusters are a minimum estimate of the length of axial melt lenses underlying this section of the SEIR.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1002/2014GC005344</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Geophysical Union</dc:publisher>
  <dc:title>Correlated patterns in hydrothermal plume distribution and apparent magmatic budget along 2500 km of the Southeast Indian Ridge</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>