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dc.contributor.author Moskalenko, V N
dc.contributor.author Murdmaa, Ivar O
dc.contributor.author Artemenko, V I
dc.contributor.author Esin, N V
dc.contributor.author Levchenko, Oleg V
dc.contributor.author Platonova, E V
dc.coverage.spatial LATITUDE: 44.232800 * LONGITUDE: 38.564200 * DATE/TIME START: 2001-07-01T00:00:00 * DATE/TIME END: 2001-07-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.125 m * MAXIMUM DEPTH, sediment/rock: 1.175 m
dc.date.accessioned 2019-11-23T10:15:31Z
dc.date.available 2019-11-23T10:15:31Z
dc.date.issued 2006-10-23
dc.identifier https://doi.pangaea.de/10.1594/PANGAEA.793022
dc.identifier https://doi.org/10.1594/PANGAEA.793022
dc.identifier.citation Moskalenko, V N; Murdmaa, Ivar O; Artemenko, V I; Esin, N V; Levchenko, Oleg V; Platonova, E V (2006): Slumping processes on the Caucasian continental slope of the Black Sea. Lithology and Mineral Resources, 41(2), 187-194, https://doi.org/10.1134/S0024490206020076
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/7279
dc.description.abstract New results of geomorphological, seismoacoustic, and lithological investigations on the upper continental slope off the Arkhipo-Osipovka Settlement are presented. Here, a large submarine slump was discovered by seismic survey in 1998. The assumed slump body, up to 200 m thick, rises 50-60 m above the valley floor that cuts the slope. Recent semiliquid mud that overlies laminated slope sediments with possible slump deformations flows down in the valley thalweg. Radiocarbon age inversion recorded in a Holocene sediment section of shelf facies recovered from the upper slope points to the gravity dislocation of sediments.
dc.format text/tab-separated-values, 120 data points
dc.language.iso en
dc.publisher PANGAEA
dc.rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
dc.rights Access constraints: unrestricted
dc.source Supplement to: Moskalenko, V N; Murdmaa, Ivar O; Artemenko, V I; Esin, N V; Levchenko, Oleg V; Platonova, E V (2006): Slumping processes on the Caucasian continental slope of the Black Sea. Lithology and Mineral Resources, 41(2), 187-194, https://doi.org/10.1134/S0024490206020076
dc.subject Ak-509
dc.subject Archive of Ocean Data
dc.subject ARCOD
dc.subject Black Sea
dc.subject DEPTH, sediment/rock
dc.subject GC
dc.subject Gravity corer
dc.subject Size fraction < 0.001 mm, clay
dc.subject Size fraction < 0.010 mm
dc.subject Size fraction > 0.100 mm
dc.subject Size fraction 0.005-0.001 mm
dc.subject Size fraction 0.010-0.005 mm
dc.subject Size fraction 0.050-0.010 mm
dc.subject Size fraction 0.100-0.050 mm
dc.subject Water content, wet mass
dc.title Slumping processes on the Caucasian continental slope of the Black Sea.
dc.title.alternative (Table) Grain size distribution of sediments from core Ak-509, Black Sea continental slope
dc.type Dataset


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