IMBRICATE THRUST STRUCTURE OF THE NORTHWESTERN CAUCASUS

dc.contributor.author	Popkov V.I.
dc.date.accessioned	2024-11-02T11:08:00Z
dc.date.available	2024-11-02T11:08:00Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13524545
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 8, 1222-1224
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46395
dc.description.abstract	Many geologists suggest a determinative role of folding in the formation of the Northwestern Caucasus structure. Mapped or drilled thrusts are considered minor structures complicating steep fold limbs. Moreover, they are often described as reverse or even normal faults. In accordance with the generally accepted concept of overthrusts as subordinate structures relative to faulting, they are shown as short unlinked segments, which do not extend beyond anticlinal folds.
dc.subject	Caucasus
dc.title	IMBRICATE THRUST STRUCTURE OF THE NORTHWESTERN CAUCASUS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06080137

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