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.
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(Archived) Without section
References
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- 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.
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- Strakhov N. M. Fundamentals of the Theory of Lithogenesis. V. 2. Gosgeolizdat, 1960, pp. 1-574.
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