title: Mineral composition of lake Sabakty sediments as an indicator of paleoclimate, Southern Urals, Russia
abstract: Relevance. Reconstruction of climatic changes based on the lacustrine sediments of lakes makes it possible to identify climatic trends and events in the late Quaternary. The Urals is considered as one of the climatic divisions, therefore, studies of the conditions of lake sedimentation, including climatic ones, are relevant in this area. Aim. To study mineral composition as an indicator of paleoclimate of Lake Sabakty sediments. Object. Core of Lake Sabakty sediments (length is 298 cm). The age 
journal: Bulletin of the Tomsk Polytechnic University Geo Assets Engineering