The article presents the results of the analysis of some geochemical features of the clayey rocks of the Suirovo Formation (Bashkirian meganticlinorium, Southern Urals). It is shown that the Zr/Sc and Th/Sc ratios in mudstones, as well as a number of lithochemical modules, gives reason to believe that thin-grained aluminosilicoclastics of the first sedimentation cycle prevails in their composition. The distribution of the mudstone data points on the La/Sc — Th/Co and Cr/Th — Th/Sc diagrams indicates the presence of a noticeable part of the products of destruction of the basic igneous rocks. The same can be assumed on the basis of their inherent average values (La/Yb)N and Eu/Eu*. Localization of the mudstone data points on the (La/Yb)N — Eu/Eu* diagram with fields characterizing the composition of the fine-grained suspension of the estuarine parts of modern rivers of different categories suggests that the provenances of the Suirovo basin were composed of a diverse complex of rocks (sedimentary rocks, acidic and basic igneous and volcanic rocks), and the rivers that transported thin-grained aluminosilicoclastics were classified as large. On the Th — La — Sc diagram, the mudstone data points tend to the field of compositions typical of oceanic island arcs, which is consistent with their position on the (Fe2O3* + MgO) — Al2O3/SiO2 diagram.
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