Journal article Open Access

Late Pleistocene channel–levee development on Monterey submarine fan, central California

Normark, W. R.


DataCite XML Export

<?xml version='1.0' encoding='utf-8'?>
<resource xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://datacite.org/schema/kernel-4" xsi:schemaLocation="http://datacite.org/schema/kernel-4 http://schema.datacite.org/meta/kernel-4.1/metadata.xsd">
  <identifier identifierType="URL">https://zenodo.org/record/1232699</identifier>
  <creators>
    <creator>
      <creatorName>Normark, W. R.</creatorName>
      <givenName>W. R.</givenName>
      <familyName>Normark</familyName>
    </creator>
  </creators>
  <titles>
    <title>Late Pleistocene channel–levee development on Monterey submarine fan, central California</title>
  </titles>
  <publisher>Zenodo</publisher>
  <publicationYear>1998</publicationYear>
  <dates>
    <date dateType="Issued">1998-09-01</date>
  </dates>
  <resourceType resourceTypeGeneral="JournalArticle"/>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://zenodo.org/record/1232699</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1007/s003670050066</relatedIdentifier>
  </relatedIdentifiers>
  <rightsList>
    <rights rightsURI="https://creativecommons.org/publicdomain/zero/1.0/legalcode">Creative Commons Zero v1.0 Universal</rights>
    <rights rightsURI="info:eu-repo/semantics/openAccess">Open Access</rights>
  </rightsList>
  <descriptions>
    <description descriptionType="Abstract">Much of the modern upper (proximal) Monterey fan is a channel–levee complex, the Upper Turbidite Sequence (UTS), that was deeply eroded after the channel breached a volcanic ridge to reach a deeper base level. Ages of sediment samples collected with the ALVIN submersible from the deepest outcrop within the channel–levee system, 390 m below the adjacent western levee crest, indicate that the UTS deposits accumulated at ≥1 m ka−1 during the last 500 ka. Neogene and Early Pleistocene sediment accumulation on the fan prior to the UTS was much slower (</description>
  </descriptions>
</resource>
88
230
views
downloads
Views 88
Downloads 230
Data volume 181.0 MB
Unique views 86
Unique downloads 219

Share

Cite as