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.
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