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The topography and fluvial palaeo-structures of the Gelendzhik Bay bottom strata and adjacent water area discovered as a result of continuous seismic-acoustic profiling using the Geont-Shelf complex are reviewed. The main characteristics and parameters of the detected intra-bottom fluvial palaeo-structures are given. The assumptions about possible mechanisms of formation of the detected structures are put forward.

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On Fluvial Paleo-Structures of the Gelendzhik Bay and Adjacent Area Seabed

  • 会议论文

  • 发表日期：

    2025年

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  • M. S. Klyuev,
  • A. A. Schreider,
  • A. S. Zverev,
  • A. E. Sazhneva,
  • A. L. Brekhovskikh,
  • I. Ya. Rakitin

摘要

The topography and fluvial palaeo-structures of the Gelendzhik Bay bottom strata and adjacent water area discovered as a result of continuous seismic-acoustic profiling using the Geont-Shelf complex are reviewed. The main characteristics and parameters of the detected intra-bottom fluvial palaeo-structures are given. The assumptions about possible mechanisms of formation of the detected structures are put forward.