Abstract
Sedimentation history of the Aldan-Maya sedimentary basin was reconstructed based on the seismostratigraphic section. A total of 10 reconstructions cover the stages of formation of the main sedimentary structures - the Riphean (Late Proterozoic) Aldan and Yudoma-Maya troughs, overlying Vendian-Cambrian deposits, as well as periods of tectonic restructuring. Studies that use a seismostratigraphic section and geological data to investigate the formation of the sedimentary cover contribute to a more substantiated and visual understanding of the evolution of the structure in question over one and a half billion years.
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