Выпуск: 8 , Том: 19 , Год издания: 1978

The Lower-Middle-Devonian deposits near the r. Shinok have been described for the first time where it outcrops continuously in north-western Anuisk-Chuisk synclinorium in Gorny Altai. The analogues of Kamishenskaya Lower Devonian Suite and Kireev and Kuvash beds of Middle Devonian age have been separated. The peculiarity to be very important of the section is the unique continuous alteration in the several assemblages of organic remains, which had been reconstructed for Gorny Altai by the separated sections based on stratigraphic data