<?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>H. R. Northrop</dc:contributor>
  <dc:creator>C. Gene Whitney</dc:creator>
  <dc:date>1987</dc:date>
  <dc:description>The Westwater Canyon Member of the Upper Jurassic Morrison Formation is a relatively homogeneous, hydrologically continuous 100-m-thick sequence of massive fluvial sandstone, bounded above and below by relatively heterogeneous, hydrologically discontinuous units and has served as a primary conduit for fluids within this stratigraphic interval. Patterns of mineral-fluid reactions suggest a basinwide hydrologic regime in which warm, evolved fluids migrated up-dip from the center of the basin under the influence of a regional hydraulic head. -from Authors</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.2475/ajs.287.4.353</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Journal of Science</dc:publisher>
  <dc:title>Diagenesis and fluid flow in the San Juan Basin, New Mexico - regional zonation in the mineralogy and stable isotope composition of clay minerals in sandstone.</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>