STRUCTURAL EVOLUTION OF THE TELETSK GRABEN (RUSSIAN ALTAI)

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dc.contributor.author Dehandschutter B.
dc.contributor.author Vysotsky E.
dc.contributor.author Delvaux D.
dc.contributor.author Klerkx J.
dc.contributor.author Buslov M.M.
dc.contributor.author Seleznev V.S.
dc.contributor.author Batist M.De.
dc.date.accessioned 2021-06-15T10:59:46Z
dc.date.available 2021-06-15T10:59:46Z
dc.date.issued 2002
dc.identifier https://elibrary.ru/item.asp?id=13863934
dc.identifier.citation Tectonophysics, 2002, 351, 1-2, 139-167
dc.identifier.issn 0040-1951
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/29054
dc.description.abstract Lake Teletskoye in the northeastern part of the Altai mountain range has attracted the attention of geo-scientists for a long time, because it fills an impressive tectonic depression. The lake is 77 km long and 4 km wide, and it has a maximum water depth of 325 m. The vertical offset of the basement surface is up to 3000 m. A multidisciplinary study of the Teletsk graben was carried out during the last few years, including satellite image and air photo analysis, bathymetric-, structural- and geomorphological mapping, high-resolution seismic profiling and seismic refraction. The structural study revealed that reactivation of preexisting weak basement zones is important in controlling the basin formation. These zones separate different tectonic terranes at the contact of which the Teletsk graben developed.
dc.subject Neotectonics
dc.subject Seismics
dc.subject Structural basin evolution
dc.subject Altai
dc.subject Lake Teletskoye
dc.title STRUCTURAL EVOLUTION OF THE TELETSK GRABEN (RUSSIAN ALTAI)
dc.type Статья


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