Astakhov, Anatolii S (1986): Grain properties of rock fragments from shelf bottom sediments of the Sea of Okhotsk [dataset publication series]. Pacific Oceanology Institute, Far East Branch of Russian Academy of Sciences, PANGAEA, https://doi.org/10.1594/PANGAEA.782621, Supplement to: Astakhov, AS (1986): Pozdnechetvertichnoe Osadkonakoplenie na Shel'fe Okhotskogo Morya (Late Quaternary Sediment Accumulation on the Sea of Okhotsk Shelf). Vladivostok, DVNC AN SSSR (Far East Science Center, USSR Academy of Sciences), 140 pp
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Abstract:
Grain size, shape and roundness of rock fragments, texture, composition of bottom sediments from the Sea of Okhotsk are under study. These data are compared with parameters of modern lithodynamic conditions of the sea and genetic types of deposits are identified. These criteria are used for partition of Holocene and Upper Pleistocene sediment series and for identifying conditions of their formation. Dependence of structure of different genetic types of deposits on intensity of hydrodynamic processes, of terrigenous contribution, and on direction consedimentational tectonic movements is under consideration.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 56.792266 * Median Longitude: 151.596029 * South-bound Latitude: 45.708300 * West-bound Longitude: 136.780000 * North-bound Latitude: 62.398000 * East-bound Longitude: 164.147000
Event(s):
Ast-5-26 * Latitude: 54.327000 * Longitude: 136.867000 * Elevation: -12.0 m * Location: Sea of Okhotsk * Method/Device: Multiple investigations (MULT)
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2 datasets
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Datasets listed in this publication series
- Astakhov, AS (1986): (Appendix 1) Contents, coefficients of roundness and flatness and their variations of rock fragments in 25-50 mm size fraction from shelf bottom sediments of the Sea of Okhotsk. https://doi.org/10.1594/PANGAEA.782619
- Astakhov, AS (1986): (Appendix 2) Contents, coefficients of roundness and flatness and their variations of rock fragments in 5-10 mm size fraction from shelf bottom sediments of the Sea of Okhotsk. https://doi.org/10.1594/PANGAEA.782620