<?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>Angela S. Jayko</dc:contributor>
  <dc:creator>M. Clark Blake Jr.</dc:creator>
  <dc:date>1986</dc:date>
  <dc:description>&lt;p&gt;Tectonostratigraphic terrances in northwest California and southwest Oregon record a complex history of subduction, collision, and transform faulting. During the late Jurassic Nevadan orogeny, the Elder Creek-Snow Camp and western Klamath terranes were imbricated during collision of an island-arc system with the continental margin. Subsequent collisions are recorded in the Pickett Peak (Early Cretaceous) and Yolla Bolly (middle Cretaceous) terranes.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.2113/gssgfbull.II.6.921</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Geosciences Institute</dc:publisher>
  <dc:title>Tectonic evolution of Northwest California and Southwest Oregon</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>