<?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>A. Maldonado</dc:contributor>
  <dc:contributor>F. Coumes</dc:contributor>
  <dc:contributor>H. Got</dc:contributor>
  <dc:contributor>A. Manaco</dc:contributor>
  <dc:creator>C.H. Nelson</dc:creator>
  <dc:date>1984</dc:date>
  <dc:description>The Ebro Fan System consists of en echelon channel-levee complexes, 50??20 km in area and 200-m thick. A few strong reflectors in a generally transparent seismic facies identify the sand-rich channel floors and levee crests. Numerous continuous acoustic reflectors characterize overbank turbidites and hemipelagites that blanket abandoned channel-levee complexes. The interlobe areas between channel complexes fill with homogeneous mud and sand from mass flow and overbank deposition; these exhibit a transparent seismic character. The steep continental rise and sediment 'drainage' of Valencia Trough at the end of the channel-levee complexes prevent the development of distributary channels and midfan lobe deposits. ?? 1984 Springer-Verlag New York Inc.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/BF02462457</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer-Verlag</dc:publisher>
  <dc:title>The Ebro Deep-Sea Fan system</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>