<?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>R. G. Eppinger</dc:contributor>
  <dc:contributor>K. Lason</dc:contributor>
  <dc:contributor>J. Slosarz</dc:contributor>
  <dc:contributor>M. Podemski</dc:contributor>
  <dc:creator>M.A. Chaffee</dc:creator>
  <dc:date>1994</dc:date>
  <dc:description>&lt;div class="hlFld-Abstract"&gt;&lt;p class="first last"&gt;The porphyry copper-molybdenum deposit at Myszkow, south-central Poland, lies in the Cracow-Silesian orogenic belt, in the vicinity of a Paleozoic boundary between two tectonic plates. The deposit is hosted in a complex that includes early Paleozoic metasedimentary rocks intruded in the late Paleozoic by a predominantly granodioritic pluton. This deposit exhibits many features that are typical of porphyry copper deposits associated with calc-alkaline intrusive rocks, including ore- and alteration-mineral suites, zoning of ore and alteration minerals, fluid-inclusion chemistry, tectonic setting, and structural style of veining. Unusual features of the Myszkow deposit include high concentrations of tungsten and the late Paleozoic (Variscan) age.&lt;/p&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1080/00206819409465497</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Taylor and Francis</dc:publisher>
  <dc:title>The Myszkow porphyry copper-molybdenum deposit, Poland</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>