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Alekseeva, Tatyana N; Sval'nov, Vyacheslav N (2006): Grain size composition of marine and river bottom sediments [dataset publication series]. P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, PANGAEA, https://doi.org/10.1594/PANGAEA.744333, Supplement to: Alekseeva, TN; Sval'nov, VN (2006): Grain-size parameters of marine sediments. Oceanology, 46(3), 430-439, https://doi.org/10.1134/S0001437006030155

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Abstract:
According to average grain size parameters (Kd, Kd1) recent sediments from the northern Caspian Sea and the Barents Sea shelf are similar, while sediments from the Norwegian Sea are closer to their counterparts of the World Ocean. Seaward content of subcolloidal (<0.001 mm) size fraction increases against the background of decreasing proportions of coarse- and medium-grained pelite (<0.01 mm) material.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 52.678075 * Median Longitude: 32.435904 * South-bound Latitude: 44.953300 * West-bound Longitude: -0.417400 * North-bound Latitude: 67.160100 * East-bound Longitude: 48.725000
Event(s):
Casp-59 * Latitude: 45.295300 * Longitude: 47.753000 * Location: Caspian Sea * Method/Device: Grab (GRAB)
Casp-61 * Latitude: 45.154600 * Longitude: 47.535000 * Location: Caspian Sea * Method/Device: Grab (GRAB)
Casp-62 * Latitude: 45.140300 * Longitude: 47.641300 * Location: Caspian Sea * Method/Device: Grab (GRAB)
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
3 datasets

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Datasets listed in this publication series

  1. Alekseeva, TN; Sval'nov, VN (2006): (Table 1) Grain size composition of recent bottom sediments from the northern Caspian Sea. https://doi.org/10.1594/PANGAEA.744289
  2. Alekseeva, TN; Sval'nov, VN (2006): (Table 1) Grain size composition of recent bottom sediments from the Volga River Delta. https://doi.org/10.1594/PANGAEA.744311
  3. Alekseeva, TN; Sval'nov, VN (2006): (Table 2) Grain size composition of recent bottom sediments from the Norwegian Sea. https://doi.org/10.1594/PANGAEA.744320