LEUCITE BASANITES AND POTASSIUM SHONKINITES OF THE UGLOVOE BASIN, SOUTHERN PRIMORYE

dc.contributor.author	Sakhno V.G.
dc.contributor.author	Maksimov S.O.
dc.contributor.author	Popov V.K.
dc.contributor.author	Sandimirova G.P.
dc.date.accessioned	2022-07-25T04:36:22Z
dc.date.available	2022-07-25T04:36:22Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13460583
dc.identifier.citation	Doklady Earth Sciences, 2004, 399, 9, 1322-1327
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38370
dc.description.abstract	The development of potassic alkaline magmatism in southern Primorye was expressed in eruption of olivine-picroilmenite-leucite basanite along the NE-oriented extensional structure that was regenerated in the Miocene. This event predated the regional opening of pull-apart structures and large-scale plateau-basalt volcanism. The sequence of volcanic events presented in this communication is confirmed by the K-Ar data.
dc.title	LEUCITE BASANITES AND POTASSIUM SHONKINITES OF THE UGLOVOE BASIN, SOUTHERN PRIMORYE
dc.type	Статья

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