ARCUATE CRUSTAL STRUCTURES

dc.contributor.author	Beloussov V.V.
dc.date.accessioned	2020-02-22T08:35:37Z
dc.date.available	2020-02-22T08:35:37Z
dc.date.issued	1986
dc.identifier	https://elibrary.ru/item.asp?id=31063272
dc.identifier.citation	DEVELOPMENTS IN GEOTECTONICS, 1986, 21, C, 41-61
dc.identifier.issn	0419-0254
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16040
dc.description.abstract	The orogenic ridges on continents and island arcs have a similar history of development and character of tectonic deformations. They also have much in common with the linear ridges. The arcuate shape of orogenic uplifts is associated with long geological history, during which the consecutively appearing structures overlaid one another or inherited from one another. The shape of island arcs is presumably the result of their former geological development.
dc.title	ARCUATE CRUSTAL STRUCTURES
dc.type	Статья

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