Hostname: page-component-78c5997874-ndw9j Total loading time: 0 Render date: 2024-10-31T22:57:22.985Z Has data issue: false hasContentIssue false

Late Precambrian geochronology of the European U.S.S.R.

Published online by Cambridge University Press:  01 May 2009

B. M. Keller
Affiliation:
Geological Institute of the AN USSR, Pyshevsky pereulok 7, Moscow Zh-17, U.S.S.R.
A. A. Krasnobaev
Affiliation:
Institute of Geology and Geochemistry of the AN USSR, Počtoviy pereulok 7, Sverdlovsk centre, U.S.S.R.

Abstract

Summary. The available data on radiometric dating of Riphean and Vendian deposits in the European part of the U.S.S.R. enabled us to establish the age of geochronological boundaries. The Riphean lower boundary was adopted as 1650 ± 50 Ma, the Vendian lower boundary as 650 ± 10 Ma, and the Cambrian lower boundary as 590 ± 10 Ma, making the total length of the Riphean about 1000 Ma and that of the Vendian about 60 Ma. This paper suggests a draft of the geochronological scale of the Late Precambrian.

Type
Articles
Copyright
Copyright © Cambridge University Press 1983

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Afanasiev, G. D. & Zykov, S. I. 1975. Geochronological Scale of the Phanerozoic in the Light of New Values of Decay Constants. Moscow: Nauka. (In Russian.)Google Scholar
Bekker, Yu. R. 1977. The first paleontological finds in the Riphean of the Urals. Izv. Akad. Nauk SSSR (ser. geol.) 3, 90100. (In Russian.)Google Scholar
Clauer, N. 1977. Géochimie isotopique du strontium des milieux sédimentaires. Application à la géochronologie de la couverture du craton Ouest-Africain. Strasbourg Univ. Louis Pasteur de Strasburg. Sc. geologiques, Memoire 45 256 p.Google Scholar
Cowie, Y. W. & Cribb, S. Y. 1978. The Cambrian System in Contributions to the Geological Time Scale. A.A.P.G. Studies in Geology 6, 355–62.Google Scholar
Fedonkin, M. A. 1981. Vendian White Sea Biota. Moscow: Nauka.Google Scholar
Firsov, L. V., Nikolaeva, I. V., Lebedev, Yu. N. & Solntseva, S. M. 1971. Composition, origin and absolute age of micaceous minerals of Lower Cambrian blue clays of the Baltic region. In Glauconite in recent Lower Paleozoic and Precambrian deposits, pp. 165–92. Moscow: Nauka. (In Russian.)Google Scholar
Garris, M. A. 1977. Stages of magmatism and metamorphism in the Pre-Jurassic history of the Urals and Preuralie. Moscow: Nauka. (In Russian.)Google Scholar
Garris, M. A., Kazakov, G. A., Keller, B. M., Polevaya, N. I. & Semikhatov, M. A. 1964. Geochronological scale of the Upper Proterozoic (Riphean and Vendian). In Absolute Age of Geological Formations, pp. 431–55. Moscow.Google Scholar
Geochronology of the USSR. 1973. Vol. 1. Precambrian. Leningrad: Nedra. (In Russian.)Google Scholar
Goldich, S. S. 1968. Geochronology of the Lake Superior region. Can. J. Earth Sci. 5, 715–25.Google Scholar
Gorokhov, I. M., Clauer, N., Varshavskaya, E. S., Kutyavin, E. P. & Drannik, A. S. 1979. Studies of clay minerals in Upper Precambrian series of the Ovruch range related to development of dating sedimentary rocks. In Izotopnaya geokhronologiya dokembriya, Ufa. pp. 96–9. (In Russian.)Google Scholar
Harland, B. W. 1975. The two geological time scales. Nature, Lond. 253, 505–7.CrossRefGoogle Scholar
Iskanderova, A. D., Neimark, L. A. & Polevaya, N. I. 1978. Correlation of some Proterozoic carbonate deposits of the East European platform through data obtained by the Pb-isochronous method. In Geochronology of the East European Platform and Joints of the Caucasian-Carpathian System, pp. 190–4. XIC Session. Moscow: Nauka. (In Russian.)Google Scholar
Ivanovskaya, T. A. & Smelov, S. B. 1976. Materials on the isotopic age and mineralogy of glauconite and Upper Riphean of the South Urals (the Minjar region). Lithologiya i poleznye iskopaemye 1, 147–51. (In Russian.)Google Scholar
Keller, B. M. & Krasilova, I. N. 1980. Late Precambrian geochronology. In Results of Science. Series General Geology. Vol. 2. Geochronological Scale and Principles of Its Compilation, pp. 5886. Moscow, Izdat. VINITI. (In Russian.)Google Scholar
Keller, B. M. & Yankauskas, T. V. 1980. Microfossils of the Riphean stratotype of the South Urals. Izvest. Akad. Nauk SSSR, Ser. Geol. 12, 5867. (In Russian.)Google Scholar
Krasnobaev, A. A., Ronkin, Yu. L., Lepikhina, O. P. & Mezentsev, V. N. 1979. Rb/Sr dating of Vendian deposits. In Izotopnaya geokhronologiya dokembriya, Ufa. pp. 78–9. (In Russian.)Google Scholar
Krasnobaev, A. A. 1981. Petrology and Rb-Sr geochronology of the Berdyaush massif or rapakivi (South Urals). Izv. Akad. Nauk SSSR, Ser. Geol. 1, 2137. (In Russian.)Google Scholar
Krasnobaev, A. A., Bibikova, E. V., Stepanov, A. I., Kirnozova, Yu. I., Ronkin, Yu. L., Makarov, V. A. & Lepikhina, O. P. 1982. The age of effusives of the Mashak suite and problem of the Lower-Middle Riphean radiological boundary. In Abstracts of Papers of the 23rd Session of the Absolute Age Commission. Uzhgorod. (In Russian.)Google Scholar
Leonov, Yu. G. 1980. Global orogenic events: orogenic periods and epochs of tectogenesis. Trudy GIN, Adak. Nauk SSSR, 34, 3371. (In Russian.)Google Scholar
Leonov, G. P. 1980. Historical Geology. Moscow: Moscow University Press. (In Russian.)Google Scholar
Pringle, J. R. 1972. Rb-Sr age determinations of shales associated with the Varanger Ice Age. Geol. Mag. 109, 465–72.Google Scholar
The Riphean Lower Boundary and Aphebian Stromatolites. Trudy GIN Akad. Nauk SSSR. (In Russian.)Google Scholar
Rubinshtein, M. M. 1965. Orogenic phases and periodicity of fold formation in the light of absolute geochronological data. Geotektonika 2, 2130. (In Russian.)Google Scholar
Stockwell, C. H. 1964. Principles of time-stratigraphic classification in the Precambrian. Spec. Publ. R. Soc. Can. 8.Google Scholar
Tectonic Map of Eurasia. 1966. 1:5000000. Ed. in Chief: A. L. Yanshin. Moscow: Geol. Inst. Acad. Sci. of USSR, Nauka.Google Scholar
Tugarinov, A. I. & Voitkevich, G. V. 1966. Precambrian geochronology of continents. Moscow: Nedra. (In Russian.)Google Scholar
The Use of Single Decay Constant Values in Geochronology. 1978. Izv. Akad. Nauk SSSR, Ser. Geol. 11, 148. (In Russian).Google Scholar