SLUMPING PROCESSES ON THE CAUCASIAN CONTINENTAL SLOPE OF THE BLACK SEA

Moskalenko V.N.; Artemenko V.I.; Esin N.V.; Murdmaa I.O.; Levchenko O.V.; Platonova E.V.

dc.contributor.author	Moskalenko V.N.
dc.contributor.author	Artemenko V.I.
dc.contributor.author	Esin N.V.
dc.contributor.author	Murdmaa I.O.
dc.contributor.author	Levchenko O.V.
dc.contributor.author	Platonova E.V.
dc.date.accessioned	2024-12-22T03:48:03Z
dc.date.available	2024-12-22T03:48:03Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13526491
dc.identifier.citation	Lithology and Mineral Resources, 2006, 41, 2, 187-194
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/47093
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. © Pleiades Publishing, Inc., 2006.
dc.subject	Holocene
dc.title	SLUMPING PROCESSES ON THE CAUCASIAN CONTINENTAL SLOPE OF THE BLACK SEA
dc.type	Статья
dc.identifier.doi	10.1134/S0024490206020076
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен