PROCESSES OF LITHOSPHERE EVOLUTION: NEW EVIDENCE ON THE STRUCTURE OF THE CONTINENTAL CRUST AND UPPERMOST MANTLE

dc.contributor.author	Artemieva I.M.
dc.contributor.author	Mooney W.D.
dc.contributor.author	Perchuc E.
dc.contributor.author	Thybo H.
dc.date.accessioned	2021-06-19T08:13:24Z
dc.date.available	2021-06-19T08:13:24Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=14418675
dc.identifier.citation	Tectonophysics, 2002, 358, 1-4, 1-15
dc.identifier.issn	0040-1951
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/29156
dc.description.abstract	We discuss the structure of the continental lithosphere, its physical properties, and the mechanisms that formed and modified it since the early Archean. The structure of the upper mantle and the crust is derived primarily from global and regional seismic tomography studies of Eurasia and from global and regional data on seismic anisotropy. These data as documented in the papers of this special issue of Tectonophysics are used to illustrate the role of different tectonic processes in the lithospheric evolution since Archean to present. These include, but are not limited to, cratonization, terrane accretion and collision, continental rifting (both passive and active), subduction, and lithospheric basal erosion due to a relative motion of cratonic keels and the convective mantle.
dc.subject	Lithosphere
dc.subject	Crust
dc.subject	Mantle
dc.title	PROCESSES OF LITHOSPHERE EVOLUTION: NEW EVIDENCE ON THE STRUCTURE OF THE CONTINENTAL CRUST AND UPPERMOST MANTLE
dc.type	Статья

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