V.A. Viginsky (
late Miocene - Early Pliocene
Turbidities of
In this work is researched the most
authentically studied neotectonic sedimentary filling of
Seismic studies of Tuapse trough
stratas above Maycop series have revealed local seismostratigraphic objects
identifiable as bodies of turbidity channels. These objects differ by local
propagation and predominantly localization to upper Miocene-lower Pliocene part
of a section. Lateral correlation of seismic records anomalies has allowed
mapping position of Meotitian-Pontian turbidity tongues. There are
correspondence of late Miocene turbidity channels with canyons existing in a
modern contour of
There were some segments with
similar hypsometric ratio: South-Crimean slope, East- and West-Taurian slopes
of Palaeo- Black Sea deep-water basin. These areas are expedient for detection
of palaeo-turbidity formations.