Морфогения Большого Алтая
Аннотация
The Great Altai is discordant to the structure of Central-Asian orogenic belt being the interlink between the Tien-Shan and the Sayan-Baikal-Stanovoi mountain systems. The Great Altai is characterized by complex inner zonality, which may be seen in the Mongol-Altai mountain raise and series of diagonal (N-W) and lateral ridges. The formation of the Great Altai was multistage with the consecutive interference of these orogenic zones.
Рецензия
Для цитирования:
Лузгин Б.Н. Морфогения Большого Алтая. Геоморфология. 2002;(4):14-21.
For citation:
Luzgin B.N. Morphogenesis of the Great Altai. Geomorfologiya. 2002;(4):14-21. (In Russ.)