История формирования рудоносного карста (на примере Западно-Тургайского боксито-рудного района)
Аннотация
Classical karst bauxiteferuos region in the Western Turgai is under consideration. Upper Cretaceous bauxiteferuos rocks fill numerous karst depressions of different morphology: wells, sink holes (cones), caldrons - corrosion-collapse, corrosion-suffusion, corrosion-erosion. The development of these landforms has gone through several stages. Depressions, which were formed during two or more tectonic-denudation cycles, are most rich of ore. Those, which underwent only one cycle, are more uniform and their ore reserves are lower.
Рецензия
Для цитирования:
Кустов Ю.Е. История формирования рудоносного карста (на примере Западно-Тургайского боксито-рудного района). Геоморфология. 2001;(1):53-60.
For citation:
Kustov J.E. The development history of ore-bearing karst in the West-Turgai bauxiteferuos region. Geomorfologiya. 2001;(1):53-60.
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