THE RELATIONSHIP OF RECENT VERTICAL MOVEMENTS TO THE MORPHOSTRUCTURAL PATTERN OF THE KAZAKH SHIELD

dc.contributor.author	Finko E.A.
dc.date.accessioned	2020-11-07T08:52:21Z
dc.date.available	2020-11-07T08:52:21Z
dc.date.issued	1992
dc.identifier	https://elibrary.ru/item.asp?id=31079145
dc.identifier.citation	Journal of Geodynamics, 1992, , 3, 209-214
dc.identifier.issn	0264-3707
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18675
dc.description.abstract	The geodetic data on recent vertical crustal movements within the Kazakh shields is in good correlation with its development in the Holocene (according to a study of juvenile river terraces); they point to gradual transition of the shield to the platform morphostructures of Western Siberia and a contrasting joining with the Central Asia orogenic belt. Small gradients of recent vertical movements dominate the shield. Moderate gradients are typical of local structures, whereas increased and extremely high gradients belong to active deep fault zones.
dc.subject	Holocene	en
dc.title	THE RELATIONSHIP OF RECENT VERTICAL MOVEMENTS TO THE MORPHOSTRUCTURAL PATTERN OF THE KAZAKH SHIELD
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary::Holocene	en
dc.subject.age	Кайнозой::Четвертичная::Голоцен	ru

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