Stratigraphy and geological events at the Frasnian-Famennian boundary in the Southern Urals

• Autorzy: Veimarn A. B. , Puchkov V. N. , Abramova A. N. , Artyushkova O. V. , Baryshev V. N. , Degtyaryov K. E. , Kononova L. I. , Maslov V. A , Mosejchuk V. M. , Pazukhin V. N. , Pravikova N. V. , Tevelev A. V. , Yarkova A. V.
• Języki publikacji: EN

Abstrakty

EN

Detailed biostratigraphic correlation of late Frasnian and Famennian sections in the Southern Urals shows that the key global scale events near the boundary of Frasnian and Famennian are clearly expressed in combination with important regional scale tectonic events. The maximum regression occured during triangularis zones time, being recorded as common hiatuses. The beginning of specific ultra- potassic mantle volcanism took place during the linguiformis Zone. Processes of olistostrome deposition, uplift of the Uraltau zone, the start of flysch deposition, and exhumation of the high pressure-low temperature Maksiutovo metamorphic complex also took place very close to the Frasnian-Famennian boundary, as the general regression coincided with active local tectonic movements as the Magnitogorsk island arc collised with the East European continent. The global scale events at the F-F boundary are connected with activity of the Late Devonian superplume, which encompassed a vast area of the Kazakhstanian, East European, Siberian, Gondwana and South Chinese plates.

Słowa kluczowe

EN

Frasnian-Famennian boundary; Southern Urals; conodonts; superplume

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2004
• Tom: Vol. 48, No 3
• Strony: 233--244
• Opis fizyczny: Bibliogr. 69 poz., rys.

Twórcy

autor

Veimarn A. B.

• Geological Department of the M. V., Lomonosov Moscow State University, Leninskie Gory, RU-119992 Moscow, Russia

autor

Puchkov V. N.

• Institute of Geology, Ufimian Scientific Centre of the Russian Academy of Sciences, K. Marks 16/2, RU-450000 Ufa, Russia

autor

Abramova A. N.

• Institute of Geology, Ufimian Scientific Centre of the Russian Academy of Sciences, K. Marks 16/2, RU-450000 Ufa, Russia

autor

Artyushkova O. V.

• Institute of Geology, Ufimian Scientific Centre of the Russian Academy of Sciences, K. Marks 16/2, RU-450000 Ufa, Russia

autor

Baryshev V. N.

• Institute of Geology, Ufimian Scientific Centre of the Russian Academy of Sciences, K. Marks 16/2, RU-450000 Ufa, Russia

autor

Degtyaryov K. E.

• Geological Institute of Russian Academy of Sciences, Pyzhevskiy 7, RU-109017 Moscow, Russia

autor

Kononova L. I.

• Geological Department of the M. V., Lomonosov Moscow State University, Leninskie Gory, RU-119992 Moscow, Russia

autor

Maslov V. A

• Institute of Geology, Ufimian Scientific Centre of the Russian Academy of Sciences, K. Marks 16/2, RU-450000 Ufa, Russia

autor

Mosejchuk V. M.

• Geological Enterprise ChelyabinskGeolKart, Omskaya 89, Chelyabinsk, Russia

autor

Pazukhin V. N.

• Institute of Geology, Ufimian Scientific Centre of the Russian Academy of Sciences, K. Marks 16/2, RU-450000 Ufa, Russia

autor

Pravikova N. V.

• Geological Department of the M. V., Lomonosov Moscow State University, Leninskie Gory, RU-119992 Moscow, Russia

autor

Tevelev A. V.

• Geological Department of the M. V., Lomonosov Moscow State University, Leninskie Gory, RU-119992 Moscow, Russia

autor

Yarkova A. V.

• Geological Enterprise ChelyabinskGeolKart, Omskaya 89, Chelyabinsk, Russia

• Geological Department of the M. V., Lomonosov Moscow State University, Leninskie Gory, RU-119992 Moscow, Russia

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