LOWER MIOCENE SEDIMENTS OF CENTRAL AND WESTERN CISCAUCASIA

Stolyarov A.S.; Ivleva E.I.

dc.contributor.author	Stolyarov A.S.
dc.contributor.author	Ivleva E.I.
dc.date.accessioned	2024-12-22T03:48:03Z
dc.date.available	2024-12-22T03:48:03Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13526492
dc.identifier.citation	Lithology and Mineral Resources, 2006, 41, 2, 174-186
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/47094
dc.description.abstract	The composition, structure, and geochemical properties of the thickest, relatively deep-water Lower Miocene sediments developed in western Ciscaucasia are considered. Of particular interest are materials from the Kuban superdeep borehole SG-12000 that recovered the uppermost layers of the Maikop Group at 3148-3961 m in the central Indol-Kuban Trough west of Krasnodar. However, the borehole did not penetrate the whole Lower Miocene section of the Maikop Group. Therefore, characteristics of the Maikop Group are supplemented with new materials from several other boreholes drilled in the eastern Kuban region. Thus, the typical (reference) Lower Miocene section of central and western Ciscaucasia has been sufficiently well described. © Pleiades Publishing, Inc., 2006.
dc.subject	Miocene
dc.title	LOWER MIOCENE SEDIMENTS OF CENTRAL AND WESTERN CISCAUCASIA
dc.type	Статья
dc.identifier.doi	10.1134/S0024490206020064
dc.subject.age	Cenozoic::Neogene::Miocene
dc.subject.age	Кайнозой::Неоген::Миоцен