Correlation of the eastern segment of Tethyan Upper Jyrassic reef barrier and adjacent facies (Carpathian-Crimean-Caucasian area)
Journal: Geology and Geochemistry of Combustible Minerals
Year: 2024

The spread of the Oxfordian-Valanginian facial belts of the carbonate shelf is traced on the territory of the eastern segment of Tethyan Upper Jurassic reef barrier by the results of own research and analysis of the published data. It is based on the scheme of distribution of the standard facial belts (D. Wilson, 1980). Complex correlation of the reefogenic and related deposits is done on the basis of comparison of the litofacial and micropaleontological composition. Standard biozonal scheme by