BASEMENT UPLIFT OF THE MONGOL-SIBERIAN REJUVENATED OROGEN

dc.contributor.author	Ufimtsev G.F.
dc.contributor.author	Shchetnikov A.A.
dc.date.accessioned	2021-02-18T10:34:08Z
dc.date.available	2021-02-18T10:34:08Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=13370629
dc.identifier.citation	Geology of the Pacific Ocean, 2001, 16, 5, 853-858
dc.identifier.issn	8755-755X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/25109
dc.description.abstract	The Mongol-Siberian belt of rejuvenated mountains is an ordered system of large domes, zones of linear warping, and the Baikal rift zone on the broad basement doming. Its morphology is paragenetically related to the shape and thickness of the asthenolith beneath the lithosphere of the mountain belt. Calculations of the upwarping range for the mountain belt basement due to asthenolithic activity were performed. The rated upwarping range is only part of the reason for its high position. It is supplemented with the isostatic uplift of light lithosphere geoblocks and the impact of the asthenolith's "roots" that extend far into the mantle along line 100°E.
dc.title	BASEMENT UPLIFT OF THE MONGOL-SIBERIAN REJUVENATED OROGEN
dc.type	Статья

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