Цикличное развитие рельефа Чикой-Даурского поднятия

Аннотация

A geomorphological structure is analyzed as reflected in a chronological-geomorphological map, where complexes of elementary landforms are shown in their genetic interrelation together with altitudinal characteristics. The synthesis is given, in particular, in the form of structural-numerical models, developed for morphostructures, their groups and the morphotecture as a whole; they are represented by variation series of elementary landforms elevation frequency, primarily for planation surfaces and steps in channels, according to cycles of erosion.