litosphereЛитосфераLITHOSPHERE (Russia)1681-90042500-302XA.N. Zavaritsky Institute of Geology and Geochemistrylitosphere-339Research ArticleСтатьиArticlesТЕКТОНИЧЕСКИЙ РЕЛЬЕФ ТИБЕТ-ГИМАЛАЕВУфимцевГеннадий Феодосьевичnoemail@neicon.ruИнститут земной коры СО РАНRussian Federation20040702201902315Copyright © Уфимцев Г.Ф., 20192019Уфимцев Г.Ф.Уфимцев Г.Ф.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.lithosphere.ru/jour/article/view/339

По картам масштаба 1:1000000 создана модель тектонического рельефа Тибет-Гималайского горного сооружения, включая Памир, Каракорум и восточную часть Гиндукуша. Проведено неотектоническое районирование региона и изложены основные особенности его новейшей геодинамики. Отмечено, что коллизионные явления в новейшей геодинамике свойственны южному (Гималаи) и северному (Куньлунь, Алтынтаг и Нанынань) скатам горного сооружения, а в собственном Тибетском нагорье преобладает блоковая тектоника на фоне общего изостатического поднятия.

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