The origin of boulders in the Neoproterozoic of Eastern Sayan Ranges, south‐west Siberia: Glacial transport versus winnowed concretions

Abstract

Palaeoclimate reconstructions in the Proterozoic geological record critically rely on our correct recognition of the products of glaciations (glaciogenic sediments, landforms and glaciotectonic structures) and the interpretation of genetic processes that formed these products. Diamictites are often and rather enthusiastically used as the only