Bottom sediment thickness as an indicator of edimentation rate and deposition environment on the northwestern shelf of the black sea

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dc.contributor.authorTuleneva, Nataliia Vitaliivna
dc.contributor.authorSuchkov, Igor O.
dc.contributor.authorFedoronchuk, Natalya O.
dc.contributor.authorФедорончук, Наталя Олександрівна
dc.contributor.authorФедорончук, Наталья Александровна
dc.contributor.authorСучков, Ігор Олександрович
dc.contributor.authorСучков, Игорь Александрович
dc.date.accessioned2017-12-01T12:33:07Z
dc.date.accessioned2017-12-01T12:34:03Z
dc.date.available2017-12-01T12:33:07Z
dc.date.available2017-12-01T12:34:03Z
dc.date.issued2013
dc.description.abstractThe northwestern Black Sea shelf is an outstanding area for research. On one hand, its geomorphological features and geological structure make it possible to trace the course of transgressions, and on the other hand, the place is rich in paleoanthropologic data on the adjoining land surface (Yanko-Hombach, 2011). Detailed reconstructions of its geologic history allow an understanding of the environmental influence on human development, and the results of investigation may be used to search for ancient human settlements within the shelf area now covered by sea. In this work, we present data about the distribution of thicknesses in Holocene sediments (Drevne- and Novochernomorian time) and their connection with the bottom relief of the northwestern Black Sea shelf.uk
dc.identifier.citationIGCP 610 First Plenary Conference and Field Trip, Tbilisi, Georgia, 12-12 October 2013uk
dc.identifier.urihttps://dspace.onu.edu.ua/handle/123456789/11648
dc.language.isoenuk
dc.titleBottom sediment thickness as an indicator of edimentation rate and deposition environment on the northwestern shelf of the black seauk
dc.typeArticleuk
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