Year: 2024
Pages: 49-64
UDC: 551.72, 550.4, 549.086, 551.72
Number: 2
Type: scientific article
DOI: 10.31084/2619-0087/2024-2-5
Topic: ARTICLES AND PUBLICATIONS
Authors: Dyakova, Svetlana A., Sergeeva, Nina D., Gataullin, Ruslan A., Abdeev, Timur R., Lukmanova, Milana R.
The article examines the features of the material composition of sandstones of the Staropetrovskaya Formation of the Upper Vendian, discovered in well 4 Aslykul in the Volga-Uralian area. According to the results of petrographic studies, the sandstones of the Staropetrovskaya Formation correspond to feldspathic-quartz, mesomicto-quartz, feldspathic-quartz greywackes and quartz-feldspathic greywackes, less frequently to monomineral quartz and arkoses proper. The mineral composition of the heavy fraction indicates the dominance of metamorphic rocks in the source area, with fewer rocks of felsic, basic and ultrabasic composition. For the first time, for deposits of the Staropetrovskaya Formation, along with lithological and petrographic methods for studying rocks in thin sections and quantitative and mineralogical analysis of the heavy fraction of crushed samples, a study was carried out using scanning electron microscopy in polished sections. This made it possible to identify rare earth element minerals (monazite and xenotime) in sandstones. Additional information on the mineral and geochemical composition of the rocks of the Staropetrovskaya Formation will be further used to reconstruct the composition of the feeding provinces and the conditions of the sedimentary basin in the Vendian time.
Staropetrovskaya Formation, Vendian, Volga-Uralian area, mineralogy, petrography, geochemistry, electron microscopy