<?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>James G. Moore</dc:contributor>
  <dc:creator>David L. Jones</dc:creator>
  <dc:date>1973</dc:date>
  <dc:description>&lt;p&gt;A Lower Jurassic ammonite has been found in metasiltstone&amp;nbsp;of the Boyden Cave roof pendant, south-central Sierra Nevada,&amp;nbsp;Calif. Although too poorly preserved to permit positive generic and&amp;nbsp;specific identification, its general shape, coiling, and ornamentation are&amp;nbsp;characteristic of Early Jurassic forms. Strata associated with the&amp;nbsp;fossiliferous rocks in the pendant include quartzite, andalusite hornfels,&amp;nbsp;and marble. This assemblage differs strikingly from nearby volcanic&amp;nbsp;rocks to the east, some of which in the Ritter Range pendant also&amp;nbsp;contain Lower Jurassic fossils. The presence of nonvolcanic Lower&amp;nbsp;Jurassic rocks of the Boyden Cave pendant lying west of coeval volcanic&amp;nbsp;rocks of the Ritter Range pendant is anomalous and may be the result&amp;nbsp;of large-scale tectonic dislocations.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Lower Jurassic ammonite from the south-central Sierra Nevada, California</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>