THREE STAGES OF TECTONIC EVOLUTION OF THE EARTH

dc.contributor.author	Sorokhtin O.G.
dc.contributor.author	Ushakov S.A.
dc.date.accessioned	2020-10-06T05:07:29Z
dc.date.available	2020-10-06T05:07:29Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31089079
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 4, 9-14
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17729
dc.description.abstract	Three long-lasting epochs in the earth's tectonic evolution are identified. First, the Catarchean epoch was characterized by the earth's endogenic passivity. Then, the exceptionally active Archean epoch was dominated by the tectonics of thin and light (primarily basaltic) lithospheric plates. Tectonic activity reached its peak in the late Archean epoch. Beginning with the early Proterozoic epoch and continuing to the present, the endogenic geological regime of the earth's evolution has been dominated exclusively by the tectonics of lithospheric plates.
dc.subject	Archean	en
dc.subject	Proterozoic	en
dc.title	THREE STAGES OF TECTONIC EVOLUTION OF THE EARTH
dc.type	Статья
dc.subject.age	Precambrian::Archean	en
dc.subject.age	Докембрий::Протерозой	ru
dc.subject.age	Precambrian::Proterozoic	en
dc.subject.age	Докембрий::Архей	ru

Files in this item

Files	Size	Format	View
There are no files associated with this item.