<?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>R. W. Plume</dc:creator>
  <dc:date>1996</dc:date>
  <dc:description>Regional aquifer systems in the Great Basin consist of carbonate-rock aquifers in the eastern Great Basin and basin-fill aquifers throughout the region. In the carbonate-rock aquifers, barriers to regional flow include Precambrian crystalline basement, upper Precambrian and Lower Cambrian clastic sedimentary rocks, and Jurassic to Tertiary granitic rocks. Basin-fill aquifers are connected to carbonate-rock aquifers in the eastern Great Basin and can be hydraulically connected with each other throughout the Great Basin.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/pp1409B</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Hydrogeologic framework of the Great Basin region of Nevada, Utah, and adjacent states</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>