<?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>Herman A. Karl</dc:contributor>
  <dc:creator>P.R. Carlson</dc:creator>
  <dc:date>1984</dc:date>
  <dc:description>Large volumes of fine-grained sediment have been transported to the deepbasin floor in the Bering Sea, especially during glacial low stands of sea level. Turbidity currents and several types of mass movement have been the chief transporting agents. ?? 1985 Springer-Verlag New York Inc.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/BF02281710</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Mass movement of fine-grained sediment to the basin floor, bering sea, Alaska</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>