<?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>George T. Faust</dc:creator>
  <dc:date>1978</dc:date>
  <dc:description>&lt;p&gt;In graben structures, volcanic eruptions and faulting are seldom simultaneous and often are not localized in the same place. Field studies in the Triassic basin of New Jersey have supplied evidence supporting the nonsimultaneity of volcanism and faulting in the Newark graben.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Time relation of the Watchung Basalt flows to the faulting in the Newark Graben</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>