<?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>Page C. Valentine</dc:contributor>
  <dc:contributor>T. M. Cronin</dc:contributor>
  <dc:contributor>E.C. Spiker</dc:contributor>
  <dc:contributor>B. W. Blackwelder</dc:contributor>
  <dc:contributor>D. F. Belknap</dc:contributor>
  <dc:contributor>J.F. Wehmiller</dc:contributor>
  <dc:contributor>Barney J. Szabo</dc:contributor>
  <dc:creator>Robert N. Oldale</dc:creator>
  <dc:date>1982</dc:date>
  <dc:description>&lt;p&gt;The Sankaty Head cliff exposes drift of at least two glaciations and interglacial marine deposits. Radiocarbon, amino-acid- racemization, and uranium-thorium analyses were used to determine the absolute ages of the beds. The results indicate that 1) the Sankaty Sand correlates with oxygen-isotope stage 5 (Sangamonian), 2) the underlying drift is older than stage 5 (Illinoian or older) , and 3) the overlying drift is Wisconsinan in age. -from Authors&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/0091-7613(1982)10&lt;246:SSAAAP&gt;2.0.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Geological Society of America</dc:publisher>
  <dc:title>Stratigraphy, structure, absolute age, and paleontology of the upper Pleistocene deposits at Sankaty Head, Nantucket Island, Massachusetts</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>