THE FIRST FINDING OF CARBONATITE TUFFS IN CENOZOIC BASALTIC VOLCANO OF SOUTHEASTERN PRIMORYE

dc.contributor.author	Maksimov S.O.
dc.contributor.author	Popov V.K.
dc.date.accessioned	2024-10-23T07:16:04Z
dc.date.available	2024-10-23T07:16:04Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13512629
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 617-622
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46171
dc.description.abstract	We found carbonatite tuffs among eruption products of the early Neogene Amba Volcano in southwestern Primorye. The volcanic edifice occupies an area of ~20 km2 in the middle reaches of the Amba River at a distance of 28 km from Amur Bay. The basalts of the stratovolcano base overlie the Permian carbonate and volcanosedimentary rocks and the Triassic arkose sandstones. The basalts are, in turn, overlapped by the upper Miocene volcanosedimentary rocks of the Ust-Suifun Formation and basalts of the Shufan Plateau.
dc.title	THE FIRST FINDING OF CARBONATITE TUFFS IN CENOZOIC BASALTIC VOLCANO OF SOUTHEASTERN PRIMORYE
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06040246
dc.subject.age	Кайнозой::Неоген

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