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- W2058320836 abstract "Pelagic carbonate oozes interlayered with mixed carbonate-volcanic silts and sands have been the principal sedimentary facies deposited on the northwest African continental rise during the late Quaternary. Terrigenous sediments are absent, having been trapped along the slope and upper continental rise in basins formed by islands or seamounts. Most quartz silts and kaolinite clays have probably been supplied by eolian sources, and montmorillonite clays by the diagenesis of volcanic rocks. 3.5 kHz profiles show reflectors which are generally parallel to the seafloor. Individual reflectors are traceable for hundreds of kilometers. Faunal analysis and radio-carbon dating indicate sedimentation rates of during the late Quaternary. Sedimentary parameters (mineralogy, carbonate abundance, lithology) apparently have remained unchanged during late Quaternary climatic fluctuations. Core data and bottom photographs indicate that reworking of bottom sediments has principally been by benthic organisms and occasionally by turbidity currents. Bottom currents presently are not active on the northwest African continental rise." @default.
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- W2058320836 date "1974-11-01" @default.
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- W2058320836 title "Quaternary Sedimentation on the Northwest African Continental Rise" @default.
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- W2058320836 doi "https://doi.org/10.1086/628024" @default.
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