<?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>A.H. Knoll</dc:contributor>
  <dc:contributor>R. E. Arvidson</dc:contributor>
  <dc:contributor>James W. Ashley</dc:contributor>
  <dc:contributor>J.F. Bell III</dc:contributor>
  <dc:contributor>W. M. Calvin</dc:contributor>
  <dc:contributor>P. R. Christensen</dc:contributor>
  <dc:contributor>B. C. Clark</dc:contributor>
  <dc:contributor>B. A. Cohen</dc:contributor>
  <dc:contributor>P.A. De Souza Jr.</dc:contributor>
  <dc:contributor>L. Edgar</dc:contributor>
  <dc:contributor>W. H. Farrand</dc:contributor>
  <dc:contributor>I. Fleischer</dc:contributor>
  <dc:contributor>Ralf Gellert</dc:contributor>
  <dc:contributor>M.P. Golombek</dc:contributor>
  <dc:contributor>J. Grant</dc:contributor>
  <dc:contributor>J. Grotzinger</dc:contributor>
  <dc:contributor>A. Hayes</dc:contributor>
  <dc:contributor>K. E. Herkenhoff</dc:contributor>
  <dc:contributor>J. R. Johnson</dc:contributor>
  <dc:contributor>B. Jolliff</dc:contributor>
  <dc:contributor>G. Klingelhofer</dc:contributor>
  <dc:contributor>A. Knudson</dc:contributor>
  <dc:contributor>R. Li</dc:contributor>
  <dc:contributor>T.J. McCoy</dc:contributor>
  <dc:contributor>S. M. McLennan</dc:contributor>
  <dc:contributor>D. W. Ming</dc:contributor>
  <dc:contributor>D. W. Mittlefehldt</dc:contributor>
  <dc:contributor>R.V. Morris</dc:contributor>
  <dc:contributor>J. W. Rice Jr.</dc:contributor>
  <dc:contributor>C. Schroder</dc:contributor>
  <dc:contributor>R.J. Sullivan</dc:contributor>
  <dc:contributor>A. Yen</dc:contributor>
  <dc:contributor>R.A. Yingst</dc:contributor>
  <dc:creator>S. W. Squyres</dc:creator>
  <dc:date>2009</dc:date>
  <dc:description>The Mars rover Opportunity has explored Victoria crater, a ???750-meter eroded impact crater formed in sulfate-rich sedimentary rocks. Impact-related stratigraphy is preserved in the crater walls, and meteoritic debris is present near the crater rim. The size of hematite-rich concretions decreases up-section, documenting variation in the intensity of groundwater processes. Layering in the crater walls preserves evidence of ancient wind-blown dunes. Compositional variations with depth mimic those ???6 kilometers to the north and demonstrate that water-induced alteration at Meridiani Planum was regional in scope.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.1170355</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Exploration of Victoria crater by the mars rover opportunity</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>