HOLOCENE DEFORMATION IN THE WESTERN END OF THE TUNKA SYSTEM OF RIFT BASINS

dc.contributor.author	Arzhannikova A.V.
dc.contributor.author	Larroque C.
dc.contributor.author	Arzhannikov S.G.
dc.date.accessioned	2021-12-03T04:37:48Z
dc.date.available	2021-12-03T04:37:48Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=14996452
dc.identifier.citation	Geologiya i geofizika, 2003, 44, 4, 373-379
dc.identifier.issn	0016-7886
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/32663
dc.description.abstract	We investigate the geometry and kinematics of Holocene active compressional structures in the Mondy basin and its surroundings (western termination of the Tunka system of rift basins) and continue the discussion on the M - 7 Mondy earthquake of 4 April 1950. The Holocene reverse-oblique motions along the W-E trending Mondy and Ikh-Uhgon faults are interpreted in the context'of Late Cenozoic evolution of a flower structure, on the basis of deciphered digital SPOT (10 m resolution) and Landsat (30 m resolution) imagery and field geomorphological measurements.
dc.subject	Tectonic deformation
dc.subject	fault kinematics
dc.subject	earthquake
dc.subject	strain field
dc.subject	Holocene
dc.title	HOLOCENE DEFORMATION IN THE WESTERN END OF THE TUNKA SYSTEM OF RIFT BASINS
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен	ru

Files in this item

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