geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2758Research ArticleНаучные сообщенияShort communicationsО строении глубоководного Дунайского конуса выносаOn the structure of the deep-sea fan of the Danube RiverКулаковаЛ. С.KulakovaL. S.ЛебедевЛ. И.LebedevL. I.ИГиРГИРоссия19881911202202Геоморфология7985Copyright © Кулакова Л.С., Лебедев Л.И., 20222022Кулакова Л.С., Лебедев Л.И.Kulakova L.S., Lebedev L.I.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/2758

On the basis of geoacoustic profiling data three generations have been distinguished within the deep-sea Ian of the Danube River (older than Middle Pleistocene, Middle Pleistocene, Late Pleistocene - Holocene ones). Schematic maps of the sediments thickness are compiled for the two younger generations. The principal Ian structure includes accessory `lenses of sediments, formed by the material sliding along the fan's slopes. The position of the axial trough and levees of the present-day Danube Ian appeared to be inconsisten with those of older fans due to migi ation of the Danube's mouth.

On the basis of geoacoustic profiling data three generations have been distinguished within the deep-sea Ian of the Danube River (older than Middle Pleistocene, Middle Pleistocene, Late Pleistocene - Holocene ones). Schematic maps of the sediments thickness are compiled for the two younger generations. The principal Ian structure includes accessory `lenses of sediments, formed by the material sliding along the fan's slopes. The position of the axial trough and levees of the present-day Danube Ian appeared to be inconsisten with those of older fans due to migi ation of the Danube's mouth.

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The authors declare that there are no conflicts of interest present.