TECTONIC EVOLUTION OF THE SOUTHWESTERN WALL OF THE BAIKAL RIFT ZONE

dc.contributor.author	Fedotov A.P.
dc.contributor.author	De Batist M.
dc.contributor.author	Pouls T.
dc.date.accessioned	2024-10-23T07:15:38Z
dc.date.available	2024-10-23T07:15:38Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13507245
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1053-1055
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46098
dc.description.abstract	We investigated the evolution of the southwestern wall of the Baikal Rift Zone (BRZ) based on the seismic structure of the sedimentary cover beneath Lake Khubsugul (Mongolia), a marginal member of the BRZ. The Khubsugul Depression formed along the boundary between the Riphean Tuva–Mongol microcontinent and the Early Paleozoic mobile zone. The Khubsugul Depression is a semigraben with steep western and gentle eastern walls. At present, the depression represents a lake with an average depth of approximately 140 m.
dc.subject	Baikal Rift Zone
dc.title	TECTONIC EVOLUTION OF THE SOUTHWESTERN WALL OF THE BAIKAL RIFT ZONE
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070117

Files in this item

Name: Fedo_06.pdf

Size: 120.7Kb

Format: PDF