title: The Paleogeography of the Formation of the Eocene Nummulitic Bank in Southwestern Crimea According to Lithological and Paleontological Data
abstract: The results of a comprehensive study of the Lower–Upper Ypresian boundary sediments at the Suvlu-Kaya Mountain section (Bakhchisarai region, Southwestern Crimea) are presented. The evolution of formation of the nummulitic bank in the study area is shown based on a detailed microfacies analysis. The sediments were formed on a deep shelf with depths at and below the storm wave base. It has been established that the Ypresian transgression was developed gradually, in three stages, with the maximum a
journal: Moscow University Geology Bulletin