PANTELLERITE-COMENDITE-ALKALI GRANITE ASSOCIATION OF THE PALEOGENE BIMODAL SERIES OF THE OKHOTSK-CHUKOTKA VOLCANOPLUTONIC BELT

dc.contributor.author	Polin V.F.
dc.contributor.author	Sakhno V.G.
dc.contributor.author	Ekimova N.I.
dc.contributor.author	Sandimirova G.P.
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=13512633
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 3, 412-417
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46172
dc.description.abstract	In eastern Chukotka, acid alkaline rocks of supposedly Tertiary age have been found within the Amguema–Kanchalan volcanic field (AKVF) of the Okhotsk–Chukotka volcanoplutonic belt (OCVB) during systematic prospecting as early as in the 1950s–1960s. Two main varieties mapped as comendites and alkali granites–granite porphyry have been distinguished among the rocks.
dc.subject	Paleogene
dc.title	PANTELLERITE-COMENDITE-ALKALI GRANITE ASSOCIATION OF THE PALEOGENE BIMODAL SERIES OF THE OKHOTSK-CHUKOTKA VOLCANOPLUTONIC BELT
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06030159
dc.subject.age	Cenozoic::Paleogene
dc.subject.age	Кайнозой::Палеоген

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