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Publikováno v:
In Quaternary International 2005 136(1):5-13
Autor:
De Grave, J., Buslov, M., Zykin, V., Van den haute, P., Dehandschutter, B., Delvaux, D., De Batist, M., Selegei, V.
The Altai Mountains are part of the vast intracontinental Central Asian orogenic system that formed during the Cenozoic as a distal effect of continued indentation of the Indian plate into the Eurasian continent. In the Siberian part of the Altai Mou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::9ff0f10e27b89c8c79320286b736576d
http://www.vliz.be/imisdocs/publications/228186.pdf
http://www.vliz.be/imisdocs/publications/228186.pdf