Spatial and temporal relationship of Devonian bauxites with reefs
Abstract
A striking feature of the Devonian period is the widespread occurrence of reefs, most of which are associated with geosynclinal seas. In character and size, the Devonian reefs present a rather motley picture. The largest reefs are located in the marginal parts of geosynclinal troughs.
Область исследования:
(Archived) Without section
Funding:
None
References
- Degtyarev D. D. Guiding significance of some corals of Devonian deposits of the middle course of the Ai River in the Southern Urals. - Tr. Gorno-geol. inst. of the Uralsk branch of the AS USSR, vol. 27, 1957.
- Rodchenko Y. M. Devonian reefs of the Northern Urals and their connection with bauxites. The Third Paleoecological-Lithological Session, June 8-12, 1965, Abstracts. PH UB AS USSR, 1965.
- Spassky N. Ya. Corals Rugosa in the Lower and Middle Devonian of the Urals. Journal of Mining Institute. v. 36, iss. 2, 1959.
- Strakhov N. M. Fundamentals of the Theory of Lithogenesis. V. 2. Gosgeolizdat, 1960, pp. 1-574.
- Kharin G. S. Stratigraphy of Devonian sediments of the Sayano-Altaic region. Salair. In Proceedings: Biostratigraphy of the Paleozoic of the Sayano-Altaic mountainous region. - Proc. Sib. R&D Institute of Geology, Geophysics and Mineral Raw Materials, vol. 20, 1960.
Similar articles
On the composition and age relations of dykes with mineralization at the Sokolovskoye deposit
1973 N. I. Rudenko, V. G. Lazarenkov, N. L. Shamanina
Regularities of cobalt distribution in the main minerals of ores and veins at the Sarbaisky open pit site
1973 N. L. Shamanina, N. I. Rudenko, T. A. Velikoborets