Geomorphology of the Tunka rift (South-west Pribaikalye)

• Autorzy: Shchetnikov A. A.
• Języki publikacji: EN

Abstrakty

EN

The Tunka rift consists of a system of baikal type basins and low-mountain intcrbasin ridges separating them. In the north it is surrounded by the alpine Tunka ridge and the low Olkha upland, and in the soulh by the Siberian mountains Western Khamar-Daban with volcanic plateau. This rift may be as a morphotypc of dry rift basin of the Baikal type (rift valley) because it has a full set of their typical structural elements and their unified forms. Relief of the rift and its mountain surroundings are composed of five belts: the belt of plains and the belt of tilted piedrnonts, the apical belt, the belt of slopes, and the belt of valley boltoms in its mountain frame. Instead of them there is a large group of interzonal land forms.

Słowa kluczowe

EN

structure of relief; Tunka rift valley

• Wydawca: Stowarzyszenie Geomorfologów Polskich
• Czasopismo: Landform Analysis
• Rocznik: 2008
• Tom: Vol. 6
• Strony: 47--56
• Opis fizyczny: Bibliogr. 15 poz., rys.

Twórcy

autor

Shchetnikov A. A.

• Institute of the Earths Crust, Lermontov sir. 128, 664033, Irkutsk, Russia.

Bibliografia

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