Spatial-temporal relationship between 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 varied 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. in-ta Ural'sk. f-la AN SSSR Tr. Gorno-geol. inst. of the Uralsk branch of the AS USSR, issue 27, 1957 (in Russian)
- Rodchenko Yu. M. Devonian reefs of the Northern Urals and their connection with bauxites. Tret'ya paleoekologo-litologicheskaya sessiya 8–12 iyunya 1965 g. Tez. dokladov The Third Paleoecological-Lithological Session, June 8-12, 1965, Abstracts. Izd. UF AN SSSR PH UB AS USSR, 1965 (in Russian)
- Spassky N. Ya. Corals Rugosa in the Lower and Middle Devonian of the Urals. Journal of Mining Institute Zapiski Gornogo Instituta, vol. 36, issue 2, 1959 (in Russian)
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- Kharin G. S. Stratigraphy of Devonian deposits of the Sayano-Altai region. Salair. In the collection: Biostratigraphy of the Paleozoic of the Sayano-Altai mountainous region Sb.: Biostratigrafiya paleozoya Sayano-Altaiskoi gornoi oblasti . Tr. Sibirsk. nauchno-issl. in-ta geologii, geofiziki i mineral. syr'ya Proc. Sib. R&D Institute of Geology, Geophysics and Mineral Raw Materials, issue 20, 1960 (in Russian)
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