Introduction
Transgressive system tracts [TST]
It is formed by the rise in sea level over the shelf edge and the general conditions of the transgressions. Sediment deposited on the shelf and slope sedimentation moves toward the continent as a transgressive series. TST presented retrogradatsionnym package parasikvensov characterizing transgression as the shelf and in the coastal lowlands. In zashelfovoy area due to lack of precipitation formed clay-fused incision [condensed-section deposits]. The foot of the front surface is called transgressive [transrgessive surface]. It represents the maximum flooding surface, which marks the beginning of transgression, reflected in a shift of the coastline in the ...
