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

Normark, W. R.


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  <dc:creator>Normark, W. R.</dc:creator>
  <dc:date>1998-09-01</dc:date>
  <dc:description>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 (</dc:description>
  <dc:identifier>https://zenodo.org/record/1232699</dc:identifier>
  <dc:identifier>10.1007/s003670050066</dc:identifier>
  <dc:identifier>oai:zenodo.org:1232699</dc:identifier>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>https://creativecommons.org/publicdomain/zero/1.0/legalcode</dc:rights>
  <dc:title>Late Pleistocene channel–levee development on Monterey submarine fan, central California</dc:title>
  <dc:type>info:eu-repo/semantics/article</dc:type>
  <dc:type>publication-article</dc:type>
</oai_dc:dc>
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