(Table 1) Grain size composition of recent sediments from the eastern Barents Sea shelf ...

Based on materials on geomorphology, hydrology, lithology, and sedimentation dynamics obtained during cruises of the P.P. Shirshov Institute of Oceanology in the Barents Sea, the author prepared a number of charts on content of the main particle size facies in shelf surface sediments, as well as a c...

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Bibliographic Details
Main Author: Pavlidis, Yury A
Format: Dataset
Language:English
Published: PANGAEA 1996
Subjects:
Event label
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Size fraction > 1 mm, gravel
Size fraction 1.000-0.500 mm, 0.0-1.0 phi, coarse sand
Size fraction 0.500-0.250 mm, 1.0-2.0 phi, medium sand
Size fraction 0.250-0.100 mm
Size fraction 0.100-0.050 mm
Size fraction 0.050-0.010 mm
Size fraction 0.010-0.005 mm
Size fraction 0.005-0.001 mm
Size fraction < 0.001 mm, clay
Sum
Grab
Gravity corer
Grain size analysis after Petelin 1967, Nauka, Moscow
Calculated
PS-12
PSh12
Professor Shtokman
Archive of Ocean Data ARCOD
Barents Sea
Online Access:https://dx.doi.org/10.1594/pangaea.759916
https://doi.pangaea.de/10.1594/PANGAEA.759916
Description
Summary:Based on materials on geomorphology, hydrology, lithology, and sedimentation dynamics obtained during cruises of the P.P. Shirshov Institute of Oceanology in the Barents Sea, the author prepared a number of charts on content of the main particle size facies in shelf surface sediments, as well as a chart of lithologic types of sediments in the Barents Sea. Factors of sedimentation control and basic features of distribution of sedimentary material over its bottom area are taken into consideration. ... : Supplement to: Pavlidis, Yury A (1996): Peculiarities of the distribution of surface sediments of the Barents Sea eastern part. Oceanology, 35(4), 565-572 ...

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