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Lake Baikal that occupies the central part of the Baikal Rift Zone infill three geomorphologically individual basins: Southern, Central, and Northern. The Central one is located between the delta of the Selenga River and the Ushkany Islands. A mountainous relief on its eastern coast is complicated by a chain of negative morphostructures, the largest of which are the Nalimovka, Nizhnyaya Turka, and Kotokel basins. The aim of this study is to determine conditions of Pleistocene sedimentation in these basins of the Baikal coast.

Pleistocene sedimentation and paleogeography reconstruction for the Eastern coast of the Middle Baikal