| Popis: |
Paper presents description of Balakhninsky and Rassohinsky swells, which were located in the central part of the Yenisei-Khatanga Basin by seismic and drilling data, and the results of its geological structure comparative analysis. History of swells formation discussed in de- tails, including rift initiation in the Late Permian-Early Triassic time and stages of inversion structures growth intensification in the Middle Triassic, Late Jurassic, Early Cretaceous and Cenozoic time. Asynchronous development of these structures established on the base of paleoreconstruction analysis. |
