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https://doi.org/10.1080/10889378209377177
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Cite Journal: Polar Geography and Geology |  Publication Date: Oct 1, 1982 |
Affiliation: Northeastern State University
Abstract The authors present a theory to explain the formation of a cryo‐aridic climatic belt in the Arctic during the ice ages. This belt had distinctive periglacial landscapes and was characterized by a wide distribution of cryogenic‐eolian yedoma layers of the ice‐loess type.
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