title: Structure and Formation of the Lower Cretaceous–Eocene Section in the Central Part of the Simferopol Uplift
abstract: This article provides the first detailed description of the 25-m thick Cretaceous–Eocene section near the Mazanka village and its stratigraphic subdivision. The geological history of the Simferopol Uplift was unraveled by comparison with the outcrops of the Zuya quarry and the Bodrak River basin, facies analysis, and reconstruction of the sedimentation environments. The results obtained show that the Valanginian–Early Hauterivian silty and sandy deltaic deposits of the regressive sedimentation p
journal: Učënye zapiski Kazanskogo universiteta. Seriâ  Estestvennye nauki/Učënye zapiski Kazanskogo universiteta. Seriâ Estestvennye nauki/Učenye zapiski Kazanskogo gosudarstvennogo universiteta. Seriâ Estestvennye nauki