<?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:creator>D.E. Wilhelms</dc:creator>
  <dc:date>1972</dc:date>
  <dc:description>&lt;p&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;The distribution of major &lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;physiographic&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt; provinces and geologic units of the &lt;/span&gt;&lt;span class="SpellingError SCXW260413605 BCX8"&gt;Tarant&lt;/span&gt;&lt;span class="SpellingError SCXW260413605 BCX8"&gt;ius&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt; quadrangle is determined by the five intersecting circular multi-ringed mare basin&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;s. Three basins, &lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;i&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;n probable order of decreasing age, are &lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;Tran&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;quill&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;itatis&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;, &lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;Fecun&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;ditatis&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;, Serenitatis, &lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;Nectaris&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;, and &lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;Crisiu&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;m&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;. The uplifted ring structures of the basin form terra mountains, peninsulas&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;, and islands, and the depressions&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt; between the uplifts are the major deposition sites of post&lt;/span&gt;&lt;span class="NormalTextRun SCXW260413605 BCX8"&gt;-basin terra and mare material.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/i722</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Geologic map of the Taruntius Quadrangle of the Moon</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>