<?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:creator>B. H. Lidz</dc:creator>
  <dc:date>1984</dc:date>
  <dc:description>Ranging in age from early Eocene to early Miocene and younger, pelagic foraminifers form the major component of a phenoclastic mudball within a fossiliferous turbidite. The turibidite is part of a more than 12m-thick section of biogenic deposits of middle Miocene age.-from Author</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.2113/gsjfr.14.3.213</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Oldest (Early Tertiary) subsurface carbonate rocks of St. Croix, USVI, revealed in a turbidite-mudball.</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>