Organic matter of Cretaceous bauxite-bearing sediments of the western side of the Turgai Trough
Abstract
All bauxite deposits of Northern Kazakhstan are of Mesozoic age of continental type and are represented by hydrargillitic ores. The largest of them are located within the western side and central part of the Turgai Trough and the southeastern slope of the Kazakhstan Shield (respectively, deposits of the West-Turgai, Central and Amangelda bauxite-ore districts).
Область исследования:
(Archived) Without section
Funding:
None
Similar articles
Peculiarities of gold-quartz formation manifestation in dyke rocks (on the example of gold occurrences in the North-East of the USSR)
1985 S. V. Sendek, B. B. Evangulov, V. A. Kuznetsova, K. V. Kisterov, V. I. Kulya, A. A. Fedchenko, L. N. Chernik
Geochemistry of zonal phenite halo of the Yraas massif (Maimecha-Kotui alkaline province)
1985 V. G. Lazarenkov