THE FORMATION CONDITIONS OF THE LOWER MAEOTIC OOLITE CARBONATES (CAPE KAZANTIP, CRIMEA)
Journal: Литология и полезные ископаемые / Lithology and Mineral Resources
Year: 2025

The genesis of oolitic carbonates among the sulfate-carbonate-clayey deposits of the Lower Maeotian in the sections of Cape Kazantip was investigated through detailed analysis. Laboratory studies were conducted utilizing a range of analytical techniques, including carbonate chemical analysis, optical polarisation with computer support for photography and scanning electron microscopy (SEM), energy dispersive spectroscopy (EDS), isotopy, gas chromatography (GCM), electron paramagnetic resonance (E