<?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>B.B. Hanshaw</dc:contributor>
  <dc:contributor>J.S. Herman</dc:contributor>
  <dc:contributor>J. N. Van Driel</dc:contributor>
  <dc:creator>W. Back</dc:creator>
  <dc:date>1986</dc:date>
  <dc:description>&lt;p&gt;Mixing of fresh groundwater with subterranean Caribbean seawater generates a highly reactive geochemical zone that enhances aragonite and calcite dissolution and permits neomorphism of aragonite.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/0091-7613(1986)14&lt;137:DDOAPR&gt;2.0.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>GeoScienceWorld</dc:publisher>
  <dc:title>Differential dissolution of a Pleistocene reef in the groundwater mixing zone of coastal Yucatan, Mexico</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>