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

Normark, W. R.


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{
  "description": "Much of the modern upper (proximal) Monterey fan is a channel\u2013levee 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\u2013levee system, 390 m below the adjacent western levee crest, indicate that the UTS deposits accumulated at \u22651 m ka\u22121 during the last 500 ka. Neogene and Early Pleistocene sediment accumulation on the fan prior to the UTS was much slower (", 
  "license": "https://creativecommons.org/publicdomain/zero/1.0/legalcode", 
  "creator": [
    {
      "@type": "Person", 
      "name": "Normark, W. R."
    }
  ], 
  "headline": "Late Pleistocene channel\u2013levee development on Monterey submarine fan, central California", 
  "image": "https://zenodo.org/static/img/logos/zenodo-gradient-round.svg", 
  "datePublished": "1998-09-01", 
  "url": "https://zenodo.org/record/1232699", 
  "@context": "https://schema.org/", 
  "identifier": "https://doi.org/10.1007/s003670050066", 
  "@id": "https://doi.org/10.1007/s003670050066", 
  "@type": "ScholarlyArticle", 
  "name": "Late Pleistocene channel\u2013levee development on Monterey submarine fan, central California"
}
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