Results of Cryotrasologic Indication of Paleosols Revealed to the North of the European and Western Siberian Loess Belt
作者： V. S. Sheinkman , V. P. Melnikov , S. N. Sedov , A. V. Rusakov
DOI: 10.1134/S1028334X19070274
关键词:
摘要: Rock freezing affects soil complexes with maximum temperature gradients and forms a set of the specific cryotrasologic features in solid matrix soils. Remaining unchanged, these serve as direct indirect indicators past cryogenic settings. Transformation mass at macro- micromorphological levels is related to indicators. Soil gleyzation drained positions conditioned by occurrence frozen aquicludes settings; it We revealed complex such paleosols north European Western Siberian Loess Belt used them estimate settings Late Pleistocene.
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