<?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>S.A. Kling</dc:contributor>
  <dc:contributor>R.Z. Poore</dc:contributor>
  <dc:contributor>K. McDougall</dc:contributor>
  <dc:contributor>E.C. Beutner</dc:contributor>
  <dc:creator>R. J. McLaughlin</dc:creator>
  <dc:date>1982</dc:date>
  <dc:description>Deformed sedimentary rocks assigned to the Franciscan assemblage in the King Range S of Cape Mendocino, N California, are dominantly deep-water argillite and sandstone occurring as thick- to thin-bedded, locally channelized marine turbidities of arkosic to andesitic volcaniclastic composition. The King Range appears to be a displaced terrane of oceanic basement overlain by Palaeogene(?) and Neogene sedimentary and igneous rocks of continental and oceanic derivation.-Authors</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/0016-7606(1982)93&lt;595:PMAOFR&gt;2.0.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Geological Society of America</dc:publisher>
  <dc:title>Post-middle Miocene accretion of Franciscan rocks, northwestern California.</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>