MORPHOTECTONICS OF THE MONGOLIA-SIBERIAN MOUNTAIN BELT

dc.contributor.author	Ufimtsev G.F.
dc.date.accessioned	2020-10-31T02:50:07Z
dc.date.available	2020-10-31T02:50:07Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=31085848
dc.identifier.citation	Journal of Geodynamics, 1990, , 4, 309-325
dc.identifier.issn	0264-3707
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18265
dc.description.abstract	The mountains of north-eastern Inner Asia comprise the Mongolia-Siberian orogenic belt which has a complex structure. The southern flank of the belt consists of a chain of large domal uplifts. The Baikal rift zone is located on the northern flank. The central segment is composed of zones of linear warping. The tectonic landforms rest on a large domal basement uplift. The morphology of the latter is paragenetically connected with the shape of the asthenolith underlying the belt. The neotectonic zones are also connected with the deep structure elements.The Mongolia-Siberian mountain belt is a group of orogenic forms typical of intracontinental mountain areas.
dc.title	MORPHOTECTONICS OF THE MONGOLIA-SIBERIAN MOUNTAIN BELT
dc.type	Статья

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