Abstract
Analysis of new 3D and 2D seismic data made it possible to describe in detail the continental slope relief of the northeastern part of the Black Sea, and a large number of gravitational processes of various types. It is established that the final phase of the active lithodynamic processes development is due to the NovoEvksin regression of the basin associated with the last glaciation and completed its development more than ten thousand years ago. The irregularities formed as a result of late Holocene landslides also occur, but their contribution is insignificant, and the amplitude rarely exceeds 1 m.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
