<?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.S. Thompson</dc:contributor>
  <dc:contributor>D. S. Kaufman</dc:contributor>
  <dc:contributor>Jordon Bright</dc:contributor>
  <dc:contributor>R. M. Forester</dc:contributor>
  <dc:creator>Charles G. Oviatt</dc:creator>
  <dc:date>1999</dc:date>
  <dc:description>Initial interpretation of the sediments from the Burmester core (Eardley et al. (1973). Geological Society of America Bulletin 84, 211-216) indicated that 17 deep-lake cycles, separated by shallow-lake and soil-forming intervals, occurred in the Bonneville basin during the Brunhes Chron (the last 780 x 103 yr). Our re-examination of the core, along with new sedimentological, geochronological, and paleontological data, indicate that only four deep-lake cycles occurred during this period, apparently correlative with marine oxygen-isotope stages 2, 6, 12, and 16. This interpretation suggests that large lakes formed in the Bonneville basin only during the most extensive of the Northern Hemisphere glaciations.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1006/qres.1999.2058</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Reinterpretation of the Burmester core, Bonneville basin, Utah</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>