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The paleogeodynamic conditions of redeposition of conodont elements in the late devonian-early carboniferous sediments of the Southern Urals

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Abstract

The peculiarities of conodont fauna redeposition of the Upper Devonian-Lower Carboniferous sediments from different structural-facial zones of the Southern Urals (the Zilair megasynclinorium on the western slope of the Southern Urals (paleocontinental sector) and the Magnitogorsk-Bogdanovsk graben in the central part of the Magnitogorsk megasynclinorium on the eastern slope (paleooceanic sector)) have been studied. The regularities of conodont fauna redeposition in the flysch foredeep and riftogenous depression (of graben) formed in the back of the volcanic arc after volcanism termination have been described.

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Authors and Affiliations

  1. Institute of Geology, Ufa Scientific Center, Russian Academy of Sciences, Ufa, Russia

    E. N. Gorozhanina, V. N. Pazukhin & V. N. Puchkov

Authors
  1. E. N. Gorozhanina
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  2. V. N. Pazukhin
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  3. V. N. Puchkov
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Additional information

Original Russian Text © E.N. Gorozhanina, V.N. Pazukhin, V.N. Puchkov, 2010, published in Doklady Akademii Nauk, 2010, Vol. 432, No. 2, pp. 210–214.

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Gorozhanina, E.N., Pazukhin, V.N. & Puchkov, V.N. The paleogeodynamic conditions of redeposition of conodont elements in the late devonian-early carboniferous sediments of the Southern Urals. Dokl. Earth Sc. 432, 560–564 (2010). https://doi.org/10.1134/S1028334X1005003X

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  • DOI: https://doi.org/10.1134/S1028334X1005003X

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