Морфоструктура центральной части Малоботуобинского района в позднем триасе — ранней юре

Аннотация

Results of paleo-geomorphological analysis of a region within the Siberian platform are discussed. Main morphostructural elements are identified which existed in the Rhaetic — Liassic paleorelief. Development of main morphostructures is proved to be inherited as well as the placers' formation. Main ways of minerals migration and accumulation have been traced and their connection - or the lack of connection - with known sources has been established.