<?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. Srodon</dc:contributor>
  <dc:contributor>M. Lee</dc:contributor>
  <dc:contributor>P.H. Nadeau</dc:contributor>
  <dc:contributor>H. R. Northrop</dc:contributor>
  <dc:creator>D. D. Eberl</dc:creator>
  <dc:date>1987</dc:date>
  <dc:description>The mineralogy and the origin of a suite of almost pure sericites, collected from fractures in hydrothermally altered volcanic rocks in the vicinity of the Silverton caldera in the western San Juan Mountains of Colorado, USA, are analysed.-J.A.Z.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:title>Sericite from the Silverton caldera, Colorado: correlation among structure, composition, origin, and particle thickness.</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>