geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3518Research ArticleДискуссииDiscussionsРегиональный уровень упорядоченности рельефаRegional level of relief orderlinessКазанскийБ. А.KazanskyB. A.Тихоокеанский океанологический институт ДВО РАНRussian Federation199825122023042228Copyright © Казанский Б.А., 20232023Казанский Б.А.Kazansky B.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/3518

Preliminary scheme of dynamic orderliness of Eurasia landforms and surrounding aquatic areas is given. It is based on universal principles of symmetry, decrement and hierarchy, natural geographic forms considered, and is represented by symmetric-antisymmetric two-level cells (Yin-Yanysystems) with different altitude levels (Earth's crust types) being divided by internal S-shaped boundary internal and external boundaries of in-yan systems coincide with the boundaries of tectonic regions.

Preliminary scheme of dynamic orderliness of Eurasia landforms and surrounding aquatic areas is given. It is based on universal principles of symmetry, decrement and hierarchy, natural geographic forms considered, and is represented by symmetric-antisymmetric two-level cells (Yin-Yanysystems) with different altitude levels (Earth's crust types) being divided by internal S-shaped boundary internal and external boundaries of in-yan systems coincide with the boundaries of tectonic regions.

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The authors declare that there are no conflicts of interest present.