<?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>J. A. Grow</dc:contributor>
  <dc:contributor>Kim D. Klitgord</dc:contributor>
  <dc:contributor>B.A. Swift</dc:contributor>
  <dc:creator>D. R. Hutchinson</dc:creator>
  <dc:date>1982</dc:date>
  <dc:description>&lt;p&gt;Multichannel seismic-reflection data together with two-dimensional gravity and magnetic models suggest that the crustal structure off North Carolina consists of normal continental crust landward of the Brunswick magnetic anomaly (BMA), rift-stage crust in the 80-km-wide zone between the BMA and the East Coast magnetic anomaly (ECMA), and normal oceanic crust seaward of the ECMA.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>American Association of Petroleum Geologists</dc:publisher>
  <dc:title>Deep structure and evolution of the Carolina Trough</dc:title>
  <dc:type>chapter</dc:type>
</oai_dc:dc>