2009
DOI: 10.1134/s0001437009030126
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Slump structures in quaternary slope sediments of the northern Derbent Basin (Caspian Sea)

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Cited by 3 publications
(5 citation statements)
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“…The profiles show a good range of downslope features. According to previous research [10,11], uplifts in the upper part of the western slope of the Derbent Basin do not represent individual slump bodies moving along the seafloor; nevertheless, the internal structure of the Neopleistocene sequence in this area suggests the presence of numerous intraformational slump duplexes. In the steepest part of the slope, clear indications of the disintegration of bottom deposits and collapsing and slumping processes were revealed.…”
Section: Hydrological Settingsmentioning
confidence: 78%
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“…The profiles show a good range of downslope features. According to previous research [10,11], uplifts in the upper part of the western slope of the Derbent Basin do not represent individual slump bodies moving along the seafloor; nevertheless, the internal structure of the Neopleistocene sequence in this area suggests the presence of numerous intraformational slump duplexes. In the steepest part of the slope, clear indications of the disintegration of bottom deposits and collapsing and slumping processes were revealed.…”
Section: Hydrological Settingsmentioning
confidence: 78%
“…These new seismic reflection data made it possible to reveal the structure of the upper sedimentary layer of the western slope of the Derbent Basin in greater detail. Areas with a chaotic pattern of the acoustic record are marked here, which are interpreted as a set of separate slump and landslide blocks [11]. They appear to have moved in the recent geologic past (Late Quaternary) down a relatively steep slope.…”
Section: Eastern Slopementioning
confidence: 87%
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