ТЕОРЕТИЧЕСКИЕ ОСНОВЫ МОРФОТЕКТОНИЧЕСКИХ ИССЛЕДОВАНИЙ. СТАТЬЯ 1. ГЕОМОРФОЛОГИЧЕСКИЙ ЭТАП И ОБЩАЯ МОДЕЛЬ РАЗВИТИЯ ПОДЛЕДНО-ПОДВОДНОГО РЕЛЬЕФА АНТАРКТИКИ

Abstract

The duration of neotectonic stage, of which the earth's crust movements formed the main features of present-day relief, is comparable with the lifetime of the ice cover. The landforms were developed under peculiar condition of inhibiting the lithodynamic processes of relief formation and thence are the most objective indicators of concurrent tectonic movements.