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      <header>
        <identifier>doi:10.1594/pangaea.761573</identifier>
        <datestamp>2024-06-26T04:28:51Z</datestamp>
        <setSpec>PANGAEA</setSpec>
        <setSpec>PANGAEA.REPOSITORY</setSpec>
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          <dc:title>Physical properties of 4 cores from the Bengal Fan</dc:title>
          <dc:creator>Weber, Michael E</dc:creator>
          <dc:creator>Wiedicke-Hombach, Michael</dc:creator>
          <dc:creator>Kudrass, Hermann-Rudolph</dc:creator>
          <dc:creator>Hübscher, Christian</dc:creator>
          <dc:creator>Erlenkeuser, Helmut</dc:creator>
          <dc:publisher>PANGAEA</dc:publisher>
          <dc:date>2011</dc:date>
          <dc:date>Issued: 2011</dc:date>
          <dc:relation>doi:10.1130/0091-7613(1997)025&lt;0315:agotbf&gt;2.3.co;2</dc:relation>
          <dc:subject>Piston corer (BGR type)</dc:subject>
          <dc:subject>SO93/3</dc:subject>
          <dc:subject>Sonne</dc:subject>
          <dc:description>New stratigraphic and high-resolution seismic data from the Bengal Fan indicate that the world's largest fan shows active growth during the most recent sea-level rise and the recent highstand. This unique phenomenon contradicts common sequence-stratigraphic models, and the sediment preserved provides new insight into the sedimentological response of a fan system to sea-level rise, climatic terminations, and monsoon intensity during the past climatic cycle. We present a detailed dated sequence of turbidite sedimentation based on a core transect perpendicular to the active channel-levee system in the upper mid-fan area. Between the two major terminations 1a (12 800 14C yr B.P.) and 1b (9700 14C yr B.P.), and especially at the end of the Younger Dryas, a 13-km-wide channel built up levees 50 m high. With decreasing sediment supply, continued sea-level rise, and increasing monsoon intensity during the early Holocene, turbidity currents were confined to the channel and gradually filled it. The canyon &quot;Swatch of No Ground,&quot; a shelf depocenter that serves as the source for frequent turbidity currents, and the channel-levee system provide the unique opportunity for studying an active highstand system. Many fans showed this behavior only during lowered sea-level.</dc:description>
          <dc:description>Supplement to: Weber, Michael E; Wiedicke-Hombach, Michael; Kudrass, Hermann-Rudolph; Hübscher, Christian; Erlenkeuser, Helmut (1997): Active Growth of the Bengal Fan during sea-level rise and highstand. Geology, 25(4), 315-318</dc:description>
          <dc:language>en</dc:language>
          <dc:type>Collection</dc:type>
          <dc:type>Supplementary Publication Series of Datasets</dc:type>
          <dc:format>application/zip</dc:format>
          <dc:rights>Creative Commons Attribution 3.0 Unported</dc:rights>
          <dc:rights>https://creativecommons.org/licenses/by/3.0/legalcode</dc:rights>
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