<?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>R.B. Whitmarsh</dc:contributor>
  <dc:contributor>S.A. Ali</dc:contributor>
  <dc:contributor>J.E. Boudreaux</dc:contributor>
  <dc:contributor>R. Coleman</dc:contributor>
  <dc:contributor>R.L. Fleisher</dc:contributor>
  <dc:contributor>R. Girdler</dc:contributor>
  <dc:contributor>Frank T. Manheim</dc:contributor>
  <dc:contributor>A. Matter</dc:contributor>
  <dc:contributor>C. Nigrini</dc:contributor>
  <dc:contributor>P. Stoffers</dc:contributor>
  <dc:contributor>P.R. Supko</dc:contributor>
  <dc:creator>D.A. Ross</dc:creator>
  <dc:date>1973</dc:date>
  <dc:description>Recent drilling in the Red Sea has shown that much of the basin is underlain by evaporites of a similar age to that of evaporites found in the Mediterranean Sea. These evaporites and their structural positions indicate that other brine areas are present - and, indeed, several others have been discovered.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.179.4071.377</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>AAAS</dc:publisher>
  <dc:title>Red sea drillings</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>