2017, The analysis of Permian climate and paleogeography can be useful in
forecasting of the situation in the future. The exposure characterized the
boundary between the Sakmarian and Artinian tiers and represented by
intercalation of argillites, siltstones, clays, limestones and sandstones. The
paleogeographic studies are conducted with application of magnetic methods.
The collection of 24 samples has been selected for carrying out the laboratory
magnetic and mineralogical analysis. The complex of methods includes
measurements of a magnetic susceptibility, hysteresis methods.
The Sakmara stage is characterized by stability of a magnetic susceptibility
and remanence coercivity. Throughout an artinsky century the mode of
sedimentation is fluctuate because climatic changes have influenced on different
nature processes. A possible cause of such changes is the decrease in sea level
due to mountain collision. Climate system tended to be more warming with full
degradation of the Gondwana glaciatio
2019, Balabanov Yu. P., Sungatullin R. Kh., Sungatullina G. M., Kosareva L. R., Glukhov M. S., Yakunina P. G., Zhernenkov A. O., Antonenko V. V., Сhurbanov A. A. Magnetostratigraphy of the Reference Sections of the Cisuralian Series (Permian System) // Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism. International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism (Kazan, Russia). Cham, Switzerland: Springer Geophysics, 2019. P. 317-342.