К тектонике Курил и Сахалина как фактору образования ландшафтов
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К тектонике Курил и Сахалина как фактору образования ландшафтов
Урусов В.М.; Варченко Л.И.
xmlui.dri2xhtml.METS-1.0.item-citation:
Вестник Красноярского государственного аграрного университета, 2014, , 11
Date:
2014
Abstract:
В статье приведены особенности тектоники Курил и Сахалина в сопоставлении с тектоникой соседних субрегионов. Подчёркнута ротация Больших Курил, где погружения и воздымания суши чередуются так же, как и на Сахалине и северо-востоке Хоккайдо. На Малых Курилах выражены только подводные террасы, что связано с однонаправленным погружением хребта Витязь, ускорившемся в голоцене.The peculiarities of Kurile Islands and Sakhalin tectonics in comparison with theneighboring subregiontectonics are presented in the article. The rotation of Big Kurile Islands where the land immersions and uplifts alternate the same way as on Sakhalin and the Hokkaidonortheast is emphasized. Only underwater terraces are expressed on Small Kurile Islandsthat is connected with the Vityaz ridge unidirectional immersion, accelerated in the Holocene.
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