Отражение зон разломов в рельефе восточных отрогов Кузнецкого Алатау

Аннотация

Types of bonds are considered which exist between linear landforms and tectonic zones. Two examples are given of correlation between geologic structure and tope-morphostructural situation. Based on previous experience a conclusion is made that tope-morphostructural maps give an additive reflection of geological effects. As to Kuznetsky Alatau, the most distinct structures in its topofield are those formed during the Mesozoic phase of the tectonic-magmatic activity.