Please use this identifier to cite or link to this item: http://dspace.onu.edu.ua:8080/handle/123456789/2354
Title: C14 dating and facies control of paleo-shorelines location on NW Black Sea shelf in Holocene
Authors: Kadurin, Serhii V.
Larchenkov, Yevhenii P.
Citation: ACaspian-Black Sea-Mediterranean corridor during last 30 ky: Sealevel change and human adaptive strategies (2005-2011) : VII plenary meeting and field trip INQUA 501 (Odessa, 21–28 August 2011). – Odessa : Astroprint, 2011.
Issue Date: 2011
Publisher: Astroprint
Series/Report no.: С.107-110
Abstract: The northwestern Black Sea shelf was an alluvial plain that was flooded in the course of the Late Neoeuxinian and Chernomorian transgression (Larchenov and Kadurin, 2011). The latter started ca. 9.4 ka BP (all radiocarbon dates in this paper are in non-calibrated years BP), and occurred in an oscillatory or transgressive-regressive manner. Each transgressive-regressive stage formed its own paleocoastline, which is well expressed in the shelf relief (Larchenkov and Kadurin, 2011). Because the number of samples dated by l4C from paleocoastlines is relatively small, interpolation and extrapolation methods along with facies analysis of bottom sediments are required.
Description: ЗБІРКА ТЕЗ ДОПОВІДЕЙ 7-ї КОНФЕРЕНЦІЇ ТА ПОЛЬОВИХ ЕКСКУРСІЙ ЗА ПРОЕКТОМ INQUA 501 «КАСПІЙСЬКО-ЧОРНОМОРСЬКО-СЕРЕДЗЕМНОМОРСЬКИЙ КОРИДОР УПРОДОВЖ ОСТАННІХ 30 ТИС. РОКІВ: ЗМІНИ РІВНЯ МОРЯ ТА АДАПТАЦІЇ ЛЮДИНИ» (2005-2011)21 -28 серпня, 2011 р., м. Одеса
URI: http://dspace.onu.edu.ua:8080/handle/123456789/2354
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