ka | en

Geodynamic environment aud paleoecology of upper Cretaceous-Paleogene basins of the western part of the eastern segment of Ajara-Trialeti folded zone
Author: Kakha QoiavaKeywords: Campanian-Maastrichtian, Danian, Ichnofauna.
Annotation:
The eastern segment of Ajara-Trialeti folded zone is made-up by Upper Cretaceous Coniacian-Santonian carbonate and Campanian-Maastrichtian carbonate-terrigenous deposits, Paleocene-Lower Eocene flish sediments and Middle Eocene volcanigenic-sedimentary rock units. In Campanian-Maastrichtian limestones and Danian sandstones has been determined rich ichnofauna common for abyssal-bathial deposits, which is very similar to ichnofauna of Upper Cretaceous-Eocene flish (turbiditic) deposits in Spain.
Lecture files:
აჭარა-თრიალეთის ნაოჭა ზონის აღმოსავლეთ სეგმენტის დასავლეთ ნაწილის ზედა ცარცულ-პალეოგენური აუზების გეოდინამიური გარემო და პალეოეკოლოგია [ka]Geodynamic environment aud paleoecology of upper Cretaceous-Paleogene basins of the western part of the eastern segment of Ajara-Trialeti folded zone [en]