THE REGULARITY OF VERTICAL CRUSTAL MOVEMENTS OF THE WESTERN SLOPES OF THE PETER THE GREAT RANGE

dc.contributor.author	Enman S.V.
dc.contributor.author	Raizman A.P.
dc.date.accessioned	2020-04-13T10:51:02Z
dc.date.available	2020-04-13T10:51:02Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30967934
dc.identifier.citation	JOURNAL OF GEODYNAMICS, 1988, 10, 2-4, 213-220
dc.identifier.issn	0264-3707
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16690
dc.description.abstract	The results of relevellings made in 1948 and 1969-1975 along the Obi-Hingou profile, which is a part of the Garm test area, are analysed. Different characteristics of slow movements in the separate parts of the levelling line divided by faults were obtained by using the displacement velocities of the Earth's surface in each separate section of the profile (from the results of repeated levellings). The uplift of the Peter the Great Range is determined against the background of subsidence in the Tadjik Depression. The exact values of maximum displacements ( ≈ 7 mm ) were determined and the radius of the deformation zone (12-13 km) was established for earthquakes with M = 4.5-5.
dc.title	THE REGULARITY OF VERTICAL CRUSTAL MOVEMENTS OF THE WESTERN SLOPES OF THE PETER THE GREAT RANGE
dc.type	Статья

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