<?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>T. H. Nilsen</dc:creator>
  <dc:date>1984</dc:date>
  <dc:description>Turbidites of the Upper Cretaceous Chugach terrane of southern Alaska were deposited in a trench during northward-directed subduction. The fault-bounded outcrop belt of the Chugach terrane is about 2000-km long and 100-km wide and was accreted to Alaska during the Cenozoic. Turbidites are at least 5000 m thick, are extensively deformed, have been regionally metamorphosed, and have been intruded by anatectic granites. Facies associations indicate an east-to-west progression from inner-fan to middle-fan, outer-fan, fan-fringe, and basin-plain deposits. To the north is a marginal trench-slope facies association and a basin. ?? 1984 Springer-Verlag New York Inc.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/BF02462465</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer-Verlag</dc:publisher>
  <dc:title>Trench-fill submarine-fan facies associations of the Upper Cretaceous Chugach terrane, southern Alaska</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>