<?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>Gordon E. Brown Jr.</dc:contributor>
  <dc:contributor>D.K. Bird</dc:contributor>
  <dc:contributor>R. H. Jahns</dc:contributor>
  <dc:contributor>E.E. Foord</dc:contributor>
  <dc:contributor>J.E. Shigley</dc:contributor>
  <dc:contributor>L.B. Spaulding Jr.</dc:contributor>
  <dc:creator>L.A. Stern</dc:creator>
  <dc:date>1986</dc:date>
  <dc:description>Several layered pegmatite-aplite intrusives exposed at the Little Three mine, Ramona, display closely associated fine-grained to giant-textured mineral assemblages which are believed to have co-evolved from a hydrous aluminosilicate residual melt with an exsolved supercritical vapour phase. Calculations of phase relations between the major pegmatite-aplite mineral assemblages and supercritical aqueous fluid were made, assuming equilibrium and closed-system behaviour as a first-order model.-J.A.Z.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:title>Mineralogy and geochemical evolution of the Little Three pegmatite-aplite layered intrusive, Ramona, California</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>