The depression type of the Upper Visean-Serpukhovian succession in the Subpolar Urals

Abstract

The Upper Visean-Serpukhovian deep-water shelf succession is described in the Subpolar Urals. Turbidite model of the sequence forming and direction of the carbonate material transport are proposed. The bioherm and shoal facial belt of the shelf margin is supposed as a main source of the material.

Keywords

• приполярный урал
• нижний карбон
• стратиграфия
• бассейн осадконакопления
• карбонатные турбидиты
• subpolar urals
• lower carboniferous
• stratigraphy
• sedimentary basin
• carbonate turbidites