Stratigraphy, Tectono-Stratigraphic Systems, and Paleogeography of the Uda and Torom Sedimentary Basins (Far East of Russia)

Resumo

The stratigraphic succession of the Mesozoic suites in the Uda and Torom sedimentary basins and the hiatuses and unconformities in the section and their duration are analyzed. The tectono-stratigraphic systems are distinguished with respect to the regional and global geological events, which makes it possible to trace the evolution of these fragments in the continental margin in the Mesozoic, as well as to propose paleogeographic and paleogeodynamic reconstructions.