<?xml version='1.0' encoding='utf-8'?>
<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>W. C. Schwab</dc:contributor>
  <dc:contributor>Richard D. Ballard</dc:contributor>
  <dc:contributor>J.L. Cheminee</dc:contributor>
  <dc:contributor>Jean Francheteau</dc:contributor>
  <dc:contributor>R. Hekinian</dc:contributor>
  <dc:contributor>D.K. Blackman</dc:contributor>
  <dc:contributor>Haraldur Sigurdsson</dc:contributor>
  <dc:creator>E. Uchupi</dc:creator>
  <dc:date>1988</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Still photographs and video images collected along the Neovolcanic Zone of the East Pacific Rise from 10&amp;deg;15&amp;prime;N to 11&amp;deg;53&amp;prime;N show that recent volcanic sheet flows, possibly less than 100 years old, are superimposed on an older sediment-laden pillow terrane. This recent activity is restricted to a narrow zone that crosses two topographic highs at 10&amp;deg;55&amp;prime;N and 11&amp;deg;26&amp;prime;N and diminishes along-axis away from these highs. The association of recent sheet flows with older flows and collapse structures on the overlapping spreading centers at 11&amp;deg;45&amp;prime;N supports the evolutionary model for the occurrence and evolution of overlapping spreading centers by MacDonald and others (1986, 1988).&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/BF02326089</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer</dc:publisher>
  <dc:title>An Angus/Argo study of the neovolcanic zone along the East Pacific rise from the Clipperton fracture zone to 12°N</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>