The Upper Ordovician of northeastern Gorny Altai: Stratigraphy and deposition environments |
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Authors: | N.V. Sennikov O.T. Obut T.Yu. Tolmacheva E.V. Lykova R.A. Khabibulina |
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Affiliation: | 2. Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia;3. Karpinsky Russian Geological Research Institute (VSEGEI), Federal Agency of Mineral Resources, Srednii pr. 74, St. Petersburg, 199106, Russia |
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Abstract: | Comprehensive lithofacies and biofacies analysis provided constraints on the origin of Upper Ordovician clastic and carbonate deposits in northeastern Gorny Altai, which form large low-elevated flat carbonate banks located relatively close to the shore. The sediments were deposited during the Sandbian and early-middle Katian stages, according to new conodont data. Upper Ordovician sections in northeastern Gorny Altai store record of two global regressions: the early Sandbian (Vollen Lowstand) and early Katian (Frognerkilen Lowstand) events. |
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Keywords: | Ordovician facies deposition environment conodonts Gorny Altai |
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